east - swrcb.ca.gov
TRANSCRIPT
C
100 80 60 40
Calcium(Ca)
ps? o
East Side Wells
Legend
6 Nitrate Concentration
J ( mg /L )
%sv x < 22.5
?°y ;_ 22.5 - 36
36 - 45 G
- , 45-90 42,
c >90
Well Depth (ft)
v
20 0 o 20 40 60
Chloride(CI) + Fluoride(F)
80
Figure 26. Piper Plot for East Side Subarea wells sampled by the CCGC. Arrows indicate the hypothesized general direction of geochemical evolution along the groundwater flow.
100
Well depths posted on the Piper diagrams (Figures 23 - 26) show generally increasing well depths from south to north. In the Upper Valley area, all posted well depths are 100 feet. In the Forebay diagram, well depths are deeper than in the Upper Valley Subarea and range from 120 to 410 feet. The well depths in the Eastside Subarea are generally deeper that the in the Forebay and Upper Valley subareas and range from 180 to over 660. In the Forebay, Eastside and Upper Valley subareas, there is no apparent relation of water type to well depth. In the Pressure Subarea, wells are generally deeper than in the Upper Valley and Forebay subareas and range from 176 to 1,010 feet. The deepest wells are associated with more geochemically evolved groundwater in the calcium /magnesium- bicarbonate /carbonate sector of the central diamond.
The geochemical evolution of groundwater therefore varies by horizontal position within the Salinas Valley Groundwater Basin and well depth. Deeper wells in the Eastside and Pressure subareas collect water that is more geochemically evolved and has lower nitrate concentrations. Shallower well depths in the Forebay and Upper Valley subareas are associated with less geochemically evolved water. In all
64
subareas, less geochemically evolved groundwater is generally associated with high nitrate concentrations.
Groundwater Age Dating
Determination of the approximate age of groundwater samples provides additional insight about factors and processes affecting nitrate concentrations. Figure 27 shows the distribution of groundwater ages
for samples collected by the CCGC and Lawrence Livermore Laboratory. The majority of the samples collected in the Forebay and Upper Basin subareas indicate groundwater recharge ages less than 30 years old. Two samples indicate recharge ages between 30 and 50 years old. In contrast, the majority of the samples in the Pressure and Eastside sub -basins indicate recharge ages greater than 30 years. Two samples indicate recharge ages within the last 30 years.
Consistent with varying concentrations with depth, groundwater recharge ages are related to well depth. Recharge years of or younger than 1980 are associated with wells shallower than 400 feet. Recharge that occurred before 1970 is associated with wells deeper than 180 feet. Samples collected from the deepest wells recharged from 1963 to 1967.
65
12140'0w 121'210'0-W 12í'010V! 1
39.400`N-
38'20'071-
30.0.1-
.-31i'40011
LANGLEY AREA
G . ro Castro' Bì
Sahn
na
Wells with groundwater age values determined from Noble Gases analyses are from samples collected by the CCGC and by LLNL (Moran JE, et al 2011).
Wells with groundwater age values determined from CFC analysis were collected by the CCGC.
<< .. : +f1tiE
EAST SIDE SUBAREA-4-
CORRAL DE YIÍìRR4 AREA
PRESSURE SUBAREA
,4S
Chuatar
Gonzales
Ñ
srEkalaOe0,4.
r i, '
_ Á e
?) O R A',tr>1.=" t
25
CdR Moonty,4g
8ip4M,40,+16. Apo, 4'+t1M!Jr10 .. Big Mritati,t
. S7LA7(1 fif't!rf
p G !, `¡p 'n
y ,-.
FOREI3AY SUBAREAj -}- `. Gres
k \,. . ._ ra+« !.fr-_ / `},`,
..¡.'' ,. /0'
// F
ÿ *È 'f w,i' r
.r i.. 4, . r UPPER VALLEY SUBAREA
EXPLANATION
Noble Gas Age Q ,30yrsold
Q 30- 60yrsold
® > 60 yrs old
CFC Age
30- 50yrsold
> 60 yrs old
El Groundwater Basin
e 0 5 10 15 ltrttlrtttlttrtl Mlles
-t- 1ua' f
I twit, ¡wit G
PAN tyC1y?
.
,t, " âr i
r ',,r ów.p'.ì , ; ;- r ,
.t;
ps
CiA',%vó
é
The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 mi2 block centered over the actual well location.
Sources Eso DeLorme, USGS.''NPS Sources. Esn. USGS, NOf,A
121'í1 0'0'N 12r21 trow
Figure 27. Distribution of groundwater recharge ages.
66
1
121'00 N
P30' 2010?t
-36.0'0.1
Nitrate concentrations and oxidation -reduction potential and dissolved oxygen concentrations
Figure 28 indicates an oxidation- reduction potential (ORP) influence on nitrate concentrations and
speciation. Higher nitrate concentrations were generally associated with less reducing conditions over about 75 mV. The line delineating an ORP value of 75 mV indicates the theoretical redox potential below which nitrate is denitrified39. Where ORP values below 75 mV were measured, nitrate concentrations were lower than where ORP values were above 75 mV. Dissolved oxygen concentrations varied from 0.03 to 13.5 mg /L. There was no apparent relation between dissolved oxygen and nitrate concentrations.
700
600
500
400 E
® 300 z
1
200
100 -1- <:.
0 x, X;; ,.
-100 0 100 200 300 400 500
Pressure Subbasin
75mV
Eastside Subbasin
X Forebay Subbasín
> Upper Valley Subbasin
ORP (mV)
Figure 28. Relation of groundwater nitrate concentrations to oxidation -reduction potential for CCGC
samples.
39 Stumm W. and Morgan, J.J., 1981, Aquatic Chemistry, John Wiley and Sons, New York
67
Conclusions
Analysis and mapping of groundwater nitrate concentration data for wells that represent the domestic supply aquifers in the Salinas Valley led us to the following significant conclusions.
Based on the examination of about 6,000 well completion reports for the Salinas Valley, we identified 1,552 well completion report designated as domestic wells. Our analysis of the well completion reports indicated that the large majority of domestic wells in the Salinas Valley are screened within 400 feet of land surface. Additionally, we identified a small portion of the well completion reports provided by DWR (75 reports) designated at public supply wells. These wells are generally completed at deeper depths than the domestic wells. However, based on the small number of well completion reports designated as public supply, we surmised that most drinking water supply wells for which data are available in GeoTracker are designated as domestic wells in the DWR well completion reports. The coincidence of locations of wells sampled and locations of available well completion reports demonstrate that the CCGC sampling and inclusion of sampling results from other agencies generally adequately represents the locations where domestic wells have been installed. Two hundred and twenty -one wells on CCGC properties were sampled in the following subareas:
o Langely - 2;
o Pressure -65; o Eastside - 35
o Forebay -93; o Upper Valley -26.
Depths for all the CCGC wells sampled ranged from 60 to 1010 feet. Domestic well depths ranged from 60 to 660 feet. For 939 wells for which we determined or obtained average nitrate concentrations in the Salinas Valley, 26% had concentrations over the maximum contaminant level (MCL). Within the five subareas, the percentage of wells exceeding the MCL varied from 9% In the Langley Subarea to 51% in the Eastside Subarea. Within the Salinas Valley, 28% of the area was mapped as having nitrate concentrations over the MCL.
Within the five subareas, the percentage of the area mapped as having high nitrate concentrations varied from 0.6 % in the Langley Subarea to 11 %, 54 %, 49% and 10% In the Pressure, East Side, Forebay and Upper Valley subareas, respectively. For the domestic wells sampled on CCGC properties, 55 % had concentrations exceeding the MCL. All available wells on CCGC properties were sampled. We estimated the uncertainty In the mapped areas by determining the standard deviation of the kriged concentrations. Standard deviation values varied from less than 5 to 10 mg /L. The distribution of nitrate concentrations with depth demonstrate that In general, concentrations above the MCL prevail within 400 feet of land surface and concentrations decrease with depth below about 400 feet. Specifically:
o In the Langley Subarea, only one point, from a depth interval of 251 -300 feet, exceeded the MCL;
o In the East Side subarea, median nitrate concentrations above the MCL were observed in depth ranges 151 -200, 401 -450, and 451 -500;
o In the Pressure Subarea, median nitrate concentrations exceed the MCL in the shallow depths from 0 to 100 feet and the median nitrate concentrations from greater depths
68
were all less than the MCL; however there are sample points that exceed the MCL at most depth intervals;
o In the Forebay Subarea, median nitrate concentrations exceeded the MCL in depth ranges from 101 to 350 feet;
o In the Upper Valley Subarea, nitrate concentrations exceeded the MCL at depths shallower than 200 feet and the six sample points greater than 200 feet were all well below the MCL
Maps depicting locations of nitrate concentrations generally indicate concentrations below the MCL in the northern Pressure Subarea and in most of the Upper Valley Subarea. Concentrations above the MCL prevail throughout most of the Pressure and Eastside subareas. We incorporated the standard deviations into the mapped nitrate concentrations to provide maps that show delineations of concentration ranges at the 66% and 95% confidence intervals. The density of wells associated with the distribution of standard deviation varied by subarea. Areas where the standard deviation values are less than 5.0 mg /L correspond to areas where there are wells. Areas without wells correspond to standard deviation values greater than 5.0 mg /L.
o In the Pressure and Eastside subareas, the spatial density of wells where the standard deviation was less than 5.0 mg /L was 1 well per 25 acres.
o In the Forebay and Upper Valley subareas, the density was 1 well per 65 and 14 acres, respectively.
o These well density values appear generally sufficient for mapping of areas where groundwater is likely to be over the MCL.
As per Regional Board approval of the CCGC workplan, contour maps were initially intended to provide guidance for sampling of additional wells. Also, the contour maps were to be verified using additional samples. Since all wells were sampled, the maps were not used for this purpose or verified with additional samples. We did verify the validity of the maps using posted data from GeoTracker. The Regional Board approval of the CCGC workplan also specifies the achievement of a 95% confidence interval for the kriged maps. We have provided a map of the entire Salinas Valley that provides contour intervals at the 95% confidence level (Figure 20) that takes into account all available data.
The kriged maps provide good estimates of the distribution of the ranges of nitrate concentrations. Most of the area mapped as over the MCL, is mapped at the 95% confidence level. Almost all the area mapped as over the MCL, is mapped at the 66% confidence interval. Our maps generally agree well with GeoTracker results. Apparent discrepancies are primarily due to obfuscation and clustering in GeoTracker mapping and the resolution of the maps presented here. There are several areas where additional data will be beneficial for the characterization of groundwater quality. These include areas where there are large data gaps such as the Upper Valley Subarea and smaller areas without data points primarily in the Pressure and Eastside subareas and less so in the Forebay Subarea. Future inclusion of data collected by the USGS and Monterrey County Health Department will improve the characterization of groundwater quality for human consumption. Additionally, further analysis of additional constituents (e.g. isotopes) will provide additional insight into processes affecting nitrate concentrations in groundwater.
69
Appendix A- Nitrate Map with Posted Concentrations and Comparison of GeoTracker Sites with Nitrate Mapping
Nitrate Map with Posted Concentrations
To facilitate comparison of kriged nitrate values shown in Figure 12, we included a map of the posted values overlain on the kriged values (Figure Al). Zero values on Figure Al represent values that were less than the reporting limit.
Comparison of GeoTracker Sites with Nitrate Mapping
We compared nitrate concentrations displayed on GeoTracker with estimated concentrations shown on the groundwater nitrate map (Figure 12). Figure A2 shows the sites displayed on GeoTracker overlaid on the estimated nitrate concentration map (Figure 12). In general, for those areas where there are member parcels (Figure 2 and A3) GeoTracker results are consistent with the estimated nitrate concentrations. There are two primary reasons why the concentrations reported on the GeoTracker sites may appear to disagree with the estimated nitrate concentrations at some locations. At some of these sites, GeoTracker concentrations do agree with the estimated concentrations, but at the scale at which the maps are drawn, the agreement between the GeoTracker concentrations and the estimated concentrations is not visible. At the other GeoTracker sites, the disagreement is due to the obfuscation and clustering of well locations that occurs when viewing the sites on GeoTracker. We identified the locations (Figure A2) where there is apparent disagreement between high reported GeoTracker concentrations and the estimated concentrations. The reasons for the apparent disagreement are described below from south to north by subarea.
30'50'0"N
36'40'0'N
36'30 0"N
41
121'40"W 12130Q^1 121.20ro'W
6 4ó°l.. f,:-` 3
8 495 48 9 26 48 18 (5 weNs)
i 72 . 41
6242 68 16
5 a 19
54 -, 14428,i2 1 30
17 (6 7118 5)
2.'i 72 6ft Ú i 7 1 4 i2
eslro,Ile2Q ,*y 15 4
.Ti / 1+ 6 ? 402A
LOf,
6 24 12e1:14.11;9. 2s
3
77 fi 1 5J ) 12 ' 38
42 ¡ i 1 1 7835 4187r4
153 17 i o
0(2), 1(9), 2(5), 4, 7(2), 8(3), 11(2), 12, 13, 14,(2), 16, 19(2), 20(2), 23, 25, 26(3), 27. 36, 40, 41(2), c 45. 50. 63, 90, 284
' ,-2,4,6,7,8 { s; ' , .!
x4 » '
Only wells used for nitrate mapping are shown. Excluded wells include wells with known well depth greater than 400 feet or well use that is either irrigation or domestic /irrigation with unknown well depth.
All NO3 concentrations are rounded to the nearest integer.
-
_a.a- 44 ¿, 4 1G Y.
; . -.s.ir`., y. , .., 48 . , ir. !v
6 3 100 59 fi\ , aí ' /
SEASIDE AREA
111115
0 7447019 94 31 +i r'+ '10 30 37
1i it hr i,ó r 5
22. 90' ) _. 0
0. O. 0 41 ( wells i
4 24 Ó 1 93 40
8E
¡ (4weila)¡
21 1:13 2r 1s
65
r'? : # i
37
614
52 i 3+16 f i
-... r r
1. 1 1(e' sw' .,.
3e50.0'N
P38'40'0,35'40'01,1
71 ,r 74-` -EAST SIDE SUBAREA .`
{c±r
i 1R 1 191 tZt7 t3 ``
19 45t 14!! c 21t4 l t` r r
' -
CORRAL:'DE TIERRA AREA
1 `
41,
i 4
112 10 142 V 15 s3 4: ' ig _1
731i.
34
13
849 39 29, 93
.-.-
;id
107
.3Q 85-_ 82
0 c;nuiior
5 78 2& yp
#v. ¢ s /1+.'t , ,1:!Íj$T /'`rlj
26 `I 7i 442935. _
311072,10 88 25 : 37 2h'
1t00 44 ; vo 21 2:2. 5 "rk':,J9°
85 2 132. `3 r11, 1.i-1 49
t4 °uonzala," _ -:
.',255 - 4
19 0.5 s 264P 187 58
EXPLANATION
Wsb with Miras. Data
Estimated Nitrate Concentration mglL
N B' 22.5 mi2ss.38
rn38 45
Mil 45.90 - >90 ® Groundwater Basin
e 3
1 L Miles
121-40'0',7
8
P ESSIiRE"- ,SU BARËÁ
. 11i r1
3i 1842411 7
97
-39'30'0'N
The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 mil block centered over the actual well location.
Sources Esri Delorme,
121'30'W
USGS.:!4PS, Souerées EsY+ :75GK0
Figure Ala. Kriged nitrate concentrations, delineation of areas with varying concentration ranges, and maximum nitrate values from wells used for kriging = Pressure, East Side, and Langley Subareas.
A-2
121'30'0-W
36'30.0't1
3ú'20'0"N
36`10.0"14.,
'5 - , 7 44 \35 28 ;----
: 2U?ii;t38 25
44 6s131 25
21 15 10 44
. 2 49 112'16'° 83 11;
1. - Gonza lét; ..
250
j2e7 58 142.1 7,
28ír
85
121.20mY 121.100\V
Only wells used for nitrate mapping are shown. Excluded wells include wells with known well depth greater than 400 feet or well use that is either irrigation or domestic /irrigation with unknown well depth.
All NO3 concentrations are rounded to th nearest integer.
yt, 1 235 .
;140!irt: ,f
YY r
4
4
154 14
o$7
"<i,),11,,,,.. 1. .]J( Ir, e
: 1`,}`'s1: i-t~Q yy .
j
J 64 4.6\-, .
`,+r J`r ''' 1.
, , A .,,1:
7
s j. f t r
1 7 1
r''.1/- ;,,e, `, :j, '=jf¡f Y74 230 <-~; A`1 , A1 '' I!f.
1 ( r 1 F m f '4'4;- 3 I X-'' t ' 1.!
41 i4 79
,, w t;
03469 47 5 4F1 Jj;i - ,yr rl
j 92 1` ~°`;#`,` . 1/810ô : r f 20 ,` r f
e,,. ; r. , ,: .+ 28°, 18: i6 I . ` rta }
8 3 8
42 i 35 . 16 14d IT ;:;. . - ..
-' 1 4 ~tt . , ,, ,. ,: `.
221 1611 Fí05
1084,4117 28 143 13' \ -" .rr e
17 27 156 16 87 +:4 4 .Y : "e' -
228 1 '' .+
-,.k.- 6621 3.
2179gb [392 `31 : ,+ 3!3
415 92 :?'
t,, ?.[ 346 , , (t 257 1331/ 1 '¢J
3 ;1 iS8 112 3!5 120 4'
242 111 1 ! 6 -rt J4 260
;
6 7834.31513 239 \ 8¡' 12 2d3-12
3-0. 174 5 ?4 146 113113._-à64 146.
.0 63
F®REBÀY SUBAREA:j;i
r 'a á
y
r F ; ..^ -:rr. 4 ,, "O. .
l y .icya °st ; t
!. r
j'-
46 4
EXPLANATION
wens with Nitrate Data
Estimated Nitrate Concentration mgIL
Wig < 22.5 ri 22.5. 36
EJ 45
45.90
In> 9°
EDGroundwater Basin
e 121'30'OVw
3
Miles
61 2
0 The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 mil block centered over the actual well location.
121`20'0 V
Sources' tsrl, ueLcrme, USCiá, NPS, source
121.107w
Figure Alb. Kriged nitrate concentrations, delineation of areas with varying concentration ranges, and maximum nitrate values from wells used for kriging - Forebay Subarea.
A-3
3,3'10 0"N
3t12POY1
121050'1N 1211/0"W 120'50'0'W
+wif ....- we !. A
36.10'0N-
:Yi 0014 -
- 260
3.4° :, .., 8,3
,12 2.: l 24 t4í'11? w d 4ô
iE?
72
48
tÿ ,fie ../r
I "1,0,,, 1,
+
r
b A (
Only wells used for nitrate mapping are shown. Excluded wells include wells with known well depth greater than 400 feet or well use that is either irrigation or domestic /irrigation with unknown well depth.
All NO3 concentrations are rounded to the nearest integer.
3 f
0 4E 4
¡ fia /
..
/Ì), ;15
$ r
yed11'.,r"2s ft`c
ror-. j 1
r !."- '
J.a f 3` 1'4.;
39
rl
Jri1°. j.d
Nr ,., É; t }et lr v a/C
-1 + diu 41 Fr"
, .. t.! .-ge l; Y r (..
P r, e '1E1at,1:/ert
(V a.i..,'J NCfZ4.4 1 a.i' (' to 1 l
r v4', ,
't110'1 Vi ;F r:i+ . {. ,,
;i.^' ,..-` i fi w,
f . 4 -.
! ¡.f
ár y,r y -; ..,
,' ,;i1
i r ! 4 e.
. /"`,
,.- ,,; r
ÿr ilt )
ti fr rr j. !
r
1r: UP,PÉRVALLEY35lBAVEA
¡_ _ ÍT..f .3,r+ ' f 91:
'k;
,elJi ' . ff .á,+'
EXPLANATION
walla with Nitrate Data
Estimated Nitrate Concentration mglL M <22.5
r 22.s -36
i-1 -4s 45 8;1
lig a55
Groundwater Basin
® 0 3 6 1 t 1 i
Miles
J.
r irÿ +rr . 13
. ,rrl.
!N
l`t ,
ß
° ,> t.
J. /± . j
b f 17 r r r,, << , . Of ; ...; 1 ., a t(i _ ;..
v r 0-.403;j11.% .,,t
°;31('' w
!),r j ! ,1 " r S ' 1 t j _. r .,a' yff 'p' .. Í-td p-_:
? j , f . ! t¡ ` ' t' 'T V c
t yc° 4
The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 mil block centered over the actual well location.
Sources: ari, Delorme. USG3 NPS, Sources: Esri:USGS, NOAH
-38'20'N
-38' 10N
-30'05J
121' 10.OYJ 121.0'0V 120' 5j0.0111
Figure A1c. Kriged nitrate concentrations, delineation of areas with varying concentration ranges, and maximum nitrate values from wells used for kriging ® Upper Valley Subarea.
A-4
?,:.'40'0'N
121'40.0W 121'205 -W
LANGLEY AREA
121'00'W
GeoTracker site locations were digitized from the standard view of GeoTracker GAMA when "Wells With Results ", "Nitrate as NO3 ", "All Years ", "Groundwaster Basins ", and Salinas Valley basins are selected. The zoom level was not changed from the fixed zoom in which each basin automatically zooms. Geotracker sites may represent multiple wells due to obfuscation and clustering and may not represent the actual well locations.
T SIDE SUBARA
SEASIDE AREA
CORRAL DE TIERRA AREA
25
; : r
PRESSURE SUBAREA
36'200-14
3,3'0011
Ca[ PR n+nP.il".
ír Rtaunrae C.e! !t*t7unliTiS
ñ;ls Msu.r,:.,
c.rltli c.'
OREEAY SUBAREA
r \
EXPLANATION
GeoTracker Wells
With Nitrate Results O Non -Defect
O <22 5 mg1L
O >225mg/Lbut <45mg /L
C >45mg/L
Groundwater Basin
Estimated Nitrate Concentration mgIL
< 22.5
22.5 -36
I J 36 -45
45.90
0 3 6 9 12
I 1 1 I 1 l I i lJ_1_iJ Miles
UPPER VALLEY SUBAREA)'`.,
121,10'011/ 121'200w
fi
Sources. Eso. DeLo me, USGS. NPS
121.00....'1
Figure A2. Geolracker site locations and estimated nitrate concentrations.
A-5
ti -sc' 4U 0"tl
-3 200.11
e36'OOYd
361(r0'N
3,1' ?VON
1214001N 121" 20tnN 2 I" tirOlN
GeoTracker site locations were digitized from the standard view of GeoTracker GAMA when "Wells With Results", "Nitrate as NO3", "All Years", "Groundwaster Basins", and Salinas Valley basins are selected. The zoom level was not changed from the fixed zoom in which each basin automatically zooms. Geotracker sites may represent multiple wells due to obfuscation and clustering and may not represent the actual well locations.
CORRAL DE 'BERRA IAREA
!... PRESSURE SU -..41)1tA'ir R. ,i; t.' C-i E
pr.- o -, - V 44 ., , /. . :-
. , , .1,..,..,
.. .;.,
.. :., ,'' 2 4, , .,...4' , / -, .
.. , ' ' :4' 1 E k rikloJE r,
1 ,S ,-1;.,.
.. , ,
..,,, ..- .- - - oarks#Y7'sue AREA ,
(,); r%,..
' - - '
, 1 , - -
:.:,....
41 4.-4._ ' :f.-
: ' 40' 'all. , - .; .. ,,., ...4,--- -,-- - ,, i ip,i,,., 9 5ilii
r*,400 --te,,-,,,,li , - . i -,. i , . o ..,1, 'ki,11,-,',;!-_,: -
!*'.*SfldriO 44 ,-, 14; kgtql-.' .._,-;-;..ey, ..v. .,- -1 , .
)r).--.; ' - t.,-
''' '''.. ' '',, :',"7"--. -...05,, frLi,,, .UPpER VALLEY SUBAREA ; /
- '
i :1 :..., . , ,
Y- -IL -,-... 1-
*it. A i '
4., .., ,.. t ,
C.
Cad Lfr,rentrgas ,
asr Maputo, . "go 4.44ilyfort
- ary bibtatriPn
;
l'Atlf. IL:11E ..-38.4001 :
A 1_,
EXPLANATION
- I CCGC Member Parcels
GeoTracker Sites With NO3 Results
o Nan-Datect
o < 22 5 mg/L
O > 22 6 mg/L but < 45 mg/L
> 45 nak
EjGroundwater Basin
o 0 3 6 9 12
Miles
121401:11N
'0041 11:rnia, 1,r11/41
Sources: ES11. DeLorme, USGS4PS, Sources: Esn, USGS.
121'27Y0-W
Figure A3. Geoiracker sites and CCGC member parcel locations.
A-6
1211701N
3020014
36'00N
Upper Va lit-y
Location Z
The maximum nitrate concentration reported on GeoTracker at this location is 135 mg /L. The
GeoTracker concentration and the estimated concentration agree at this location when viewed at a
larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results ß Non -Detect
o < 22.5 mg /L
G > 22.5 mg /L but < 45 mg /L
o > 45 mg /L
Groundwater Basin
Estimated Nitrate Concentration mg /L
<22.5
f 22.5 - 36
36 -45
L__y 45 - 90
> 90
0 1,000 2,000
Feet
Location 2
There are results for 12 CDPH wells at this location south of King City where there are no CCGC member parcels. All samples for three wells were collected before 2000, so these data were excluded from our analysis. The nine remaining wells have concentrations ranging from 4.4 mg /L to 143 mg /L. Due to GeoTracker obfuscation and clustering, the location shown on GeoTracker is not accurate compared to the actual well locations used to estimate concentrations. Therefore the GeoTracker concentration and
the estimated concentration do not agree at this location. The well with a reported nitrate concentration of 143 mg /L is actually located approximately 2 miles north of the location shown on
GeoTracker and the estimated concentration agrees with the reported concentration at the mapped
well location.
Location 3
There are three CDPH supply wells at this location with a maximum concentration of 46 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a
larger scale.
EXPLLAFlRT{Oß!
GeoTracker Site
With Nitrate Results o Non -Detect
o < 22.5 mg/L
o > 22,5 mg /L but < 45 mg(L
o > 45 mg /L
_.] Groundwater Basin
Estimated Nitrate Concentration mg /L
< 22 5
22.5 - 36
r -1 36 - 45
E 145 -90
¡ >90
o 0 1,000 2,000 J 1
Feet
Upper Valley Subarea Summary
Of the five GeoTracker locations shown in the Upper Valley Subarea with concentrations over the MCL (Figure A2), four plot in an area we estimated the concentration to be above the MCL. One location plots within the area estimated to be below the MCL, however the GeoTracker location is inaccurate due to obfuscation and clustering.
Forebay Subarea
Location 4
The maximum concentration reported on GeoTracker at this location is 31 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results o Non- Detect
e < 22.5 mg /L
o > 22.5 mg /L but < 45 mg /L
© > 45 mg /L
Groundwater Basin
Estimated Nitrate Concentration mg /t,
<22.5
En 22.5 -36
r--136 -45
(!
J45 -90
1 >90
0 1,000 2,000
Feet
Forebay Subarea Summary
__J
Of the six GeoTracker locations shown in the Forebay Subarea with concentrations over the MCL (Figure A2), all six plot in an area we estimated the concentration to be above the MCL.
East Side Subarec
Location 5
There are results for 12 environmental monitoring wells at this regulated site east of Gonzales where there are no CCGC member parcels. The maximum concentration reported on GeoTracker at this location is 112.5 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site With Nitrate Results
o Non -Detect
o < 22.5 mg /L
o > 22.5 mg /L but < 45 mg /L
> 45 mg /L
[1.7:1 ] Groundwater Basin
Estimated Nitrate Concentration rmg /L.
<22.5
22.5 -36
36 -45
- 45 - 90
Eij > 90
0 500 1,000 I=
Feet ---- ------ - _
Location 6
There are two environmental monitoring wells located at this cluster site, which are associated with the Western Farm Services clean -up site that has possible nitrate contamination. Both these wells record exceedingly high nitrate values dues to this contamination. These wells were excluded from our kriging dataset (see Appendix B). Therefore, the estimated nitrate concentration does not match the maximum concentration report on GeoTracker.
Location 7
The maximum concentration reported on GeoTracker at this location is 70 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results o Non- Detect
o < 22.5 mg!L
o > 22.5 mg /L but < 45 mg!L
o > 45 mg!L
Groundwater Basin
Estimated Nitrate Concentration mg /L
J < 22.5
X22.5 -36
36 -45
45 -90
>90
0 1,000 2,000
Feet
East Side Subarea Summary
Of the 15 GeoTracker locations shown in the East Side Subarea with concentrations over the MCL
(Figure A2), fourteen plot in an area where we estimated the concentration to be above the MCL. The one GeoTracker location that plots were the estimated nitrate concentration is less than the MCL is the location where data were excluded from the kriging because the data came from wells at a groundwater nitrate clean -up site.
Pressure Subarea
Location 8
The maximum concentration reported on GeoTracker at this location is 132 mg /L. Due to GeoTracker obfuscation and clustering, the location shown on GeoTracker is not accurate compared to the actual well locations used to estimate concentrations. Therefore the GeoTracker concentration and the estimated concentration do not agree at this location, The well with a reported nitrate concentration of 132 mg /L is actually located approximately 1.1 miles east of the location shown on GeoTracker and the estimated concentration agrees with the reported concentration at the mapped well location.
Location 9
The maximum concentration reported on GeoTracker at this location is 52 mg /L. However, the well depth is greater than 400 feet and the point was excluded from the kriging. Therefore the estimated nitrate concentration shown on the map is less than the maximum value reported on GeoTracker.
A-11
Location 10 The maximum concentration reported on GeoTracker at this location is 92.6 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results o Non -Detect
O < 22.5 mg /L
O > 22.5 mg /L but < 45 mg /L
o > 45 mg /L.
Groundwater Basin
Estimated Nitrate Concentration mg /L.
L_ < 22.5
22.5 -36
El] 36 - 45
t 45 -90
>90
0 1,000 2,000 J _ I
Feet
O
Location 11 The maximum concentration reported on GeoTracker at this location is 84 mg /L. Due to GeoTracker obfuscation and clustering, the location shown on GeoTracker is not accurate compared to the actual well locations used to estimate concentrations. Therefore the GeoTracker concentration and the estimated concentration do not agree at this location. The well with a reported nitrate concentration of 84 mg /L is actually located over 2 miles east of the location shown on GeoTracker and the estimated concentration agrees with the reported concentration at the mapped well location.
Location 12 There are five environmental monitoring wells located at this cluster site. Two of these wells are found at the Western Farm Services site which has possible nitrate contamination. Both of these wells have very high reported nitrate values due to this contamination. These wells were excluded from our kriging dataset (see Appendix B). The three other wells all have non- detect values of nitrate.
Location 13 There are numerous wells located at this cluster site, some of which are associated with a fertilizer contamination site. Wells that are associated with this site and have very high reported nitrate concentrations were excluded from our kriging dataset (see Appendix B). The maximum value used in
the kriging dataset was 100 mg /l. and the maximum value in the estimate concentration map is 90 mg /L. The discrepancy is due to the close proximity of the well with the maximum concentration to wells with non -detectable nitrate concentrations. The high estimated concentration areas can be seen when viewed at a larger scale.
A-12
3
EXPLANATION
GeoTracker Site With Nitrate Results
o Non -Detect
O < 22.5 mg /L
o > 22.5 mg /L but < 45 mg /L
O > 45 mg /L
Groundwater Basin
Estimated Nitrate Concentration mg /L
<22.5
¡-; 22.5 - 36
L _ 36 - 45
45 - 90
> 90
e 0 1,000 2,000
Feet
Location 14 The maximum concentration reported on GeoTracker at this location is 50 mg /L but the sample was
collected prior to the year 2000. Therefore, the value was excluded from our kriging dataset.
Location 15 The maximum concentration reported on GeoTracker at this location is 42 mg /L. The GeoTracker
concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site With Nitrate Results
o Non-Detect
O < 22.5 mg /L
O > 22.5 mg /L but < 45 mg /L
O > 45 mg /L
Groundwater Basin f
Estimated Nitrate Concentration mg /L
< 22.5
22.5-36
L 136-45
45 - 90
> 90
0 1,000 2,000 La -J
Feet
A-13
Location 16 The maximum nitrate concentration reported on GeoTracker at this location is 33 mg /L, but the sample was collected prior to year 2000 and was therefore excluded from our dataset. The maximum nitrate concentration in the timeframe of our dataset is 15.4 mg /L. This maximum concentration and the estimated concentration agree at this location.
Location 1
The maximum nitrate concentration from the four wells reported on GeoTracker at this location is 110 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION GeoTracker Site With Nitrate Results
o Non -Detect
o < 22.5 mg /L
o > 22.5 mg /L but < 45 mg /L
o > 45 mg /L
ElGroundwater Basin
Estimated Nitrate Concentration mg /L r 22.5
t 22.5 - 36
3s -45
45 -90 ^i >90
e 0 1,000 2,000 1 J
Feet
Location 18 There are six environmental monitoring wells clustered at this location. The maximum nitrate concentration reported on GeoTracker is 72 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
A-14
EXPLANATION
GeoTrack er Site
With Nitrate Results o Non -Detect
O < 22.5 mg /L
o > 22.5 mg /L but < 45 mg /L
c > 45 mg /L
Groundwater Basin
Estimated Nitrate Concentration mg /L
1 I <22.5
m m ; 22.5 - 36
36 -45
E 45 -90
>90
o 0 1,000 2,000
Feet
Location 19 There are nine environmental monitoring wells located at this location with a maximum nitrate
concentration of 48.15 mg /L. The GeoTracker concentration and the estimated concentration agree at
this location when viewed at a larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results O Non -Detect
o <22 5 mg /L
o > 22.5 mg /L but < 45 mg /L
O > 45 mg /L
EDGroundwater Basin
Estimated Nitrate Concentration nag /L
; < 22.5
°-;j 215 . 36
1-1 36 - 45
p 45-90 L_-_-_--
>90
o 0 500 1,000
l Feet
A-15
Location 20 There are 11 CDPH supply wells at this location with a maximum concentration of 110 mg /L. However, due to GeoTracker obfuscation and clustering, the location shown on GeoTracker is not accurate compared to the actual well locations used to estimate concentrations. The high value of 110 mg /L is
actually located at Location 17. The maximum nitrate concentration from a well that is actually located at Location 20 is 46 mg /L, which agrees with our estimated concentration when viewed at a larger scale.
-
EXPLANATION GeoTracker Site With Nitrate Result.
o Non- Detect
O < 22.5 mg!L
o > 22.5 mglL but < 45 mg /L
O > 45 mg /L
( l Grounolveter Basin
Estimated Nitrate Concentration rng /L
.._ <22.5 ! 22.5-36 -- 36-45
45-90 - -
0 500 1,000
Feet
Location 21
The maximum nitrate concentration from the 29 wells reported on GeoTracker at this location is 62
mg /L. The GeoTracker concentration and the estimated concentration agree at this location when
viewed at a larger scale.
EXPLANATION
GeoTracker Site
With Nitrate Results o Non- Detect
O < 22.5 mg /L
G > 22.5 mg /L but < 45 mg /L
O > 45 mg /L R Groundwater Basin
Estimated Nitrate Concentration
mg /L
<22.5
122.5.36
=36 -45
_'.45 -90
>90
e 0 1,000 2,000 t
Feet
Pressure Subarea Summary
Of the 16 GeoTracker site shown in the Pressure Subarea with concentrations over the MCL (Figure A2),
11 plot in an area where the estimated the concentration is shown to be above the MCL. There are five
sites where GeoTracker shows a concentration greater than the MCL, but the estimated concentration is
less than the MCL. At two of the sites the discrepancy is due to obfuscation clustering of wells in
GeoTracker. At three of the sites the discrepancy is because data were excluded from the kriging dataset
due to very high concentrations from a localized contamination site or data collected prior to the year
2000.
Langley Subarea
Location 22 The maximum nitrate concentration from the 19 wells reported on GeoTracker at this location is 73 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION GeoTracker Site With Nitrate Recuits
o Non -Detect
O <22.5mgL
O > 22.5 mg /L but < 45 mg /L
O > 45 mg /L
a Groundwater Basin
Estimated Nitrate Concentration mg /L
rr < 22 5
22.5.36
36 .45
i45 -90
>90
r
0 1,000 2,000
i Feet
Location 23
There are 26 CDPH supply wells at this location with a maximum concentration of 68 mg /L. The
GeoTracker concentration and the estimated concentration agree at this location when viewed at a
larger scale.
F- 1 EXPLANATION
GeoTracker Site
With Nitrate Results o Non -Detect
O < 22.5 mg /L
O > 22.5 mg /L but < 45 mg /L
O > 45 mg /L
Groundwater Basin
Estimated Nitrate Concentration mg /L r < 22.5
L¡i 22.5 - 36
F-1 36 - 45
45 -90
)>90
0 1,000 2,000 L _lr _
Feet
Location 24
Due to GeoTracker obfuscation and clustering, the location shown on GeoTracker is not accurate
compared to the actual well locations used to estimate concentrations. The clustered well location plots
outside of the groundwater basin boundary, however these points are associated with the Langley Area
groundwater basin according to GeoTracker.
A-19
Location 25 There are 35 CDPH supply wells clustered at this location. The maximum nitrate concentration reported on GeoTracker is 67 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a larger scale.
EXPLANATION GeoTracker Site With Nitrate Results
o Non-Detect
o < 22 5 mg1L
o > 22.5 mglL but < 45 mg/L
O > 45 mg/L
Groundwater Basin
Estimated Nitrate Concentration mg/L E <22.5
¡22.5-35
36-45
F45-90 >90
o 0 1,000 2,000 I I I
Feet
Location 26 There are many environmental monitoring wells at this location, with nitrate concentrations ranging
from non -detect to 283.5 mg /L. When this location is viewed at a larger scale, the individual sites can be
seen. For almost all sites, the GeoTracker concentration and the estimated concentration agree at these
locations. The maximum concentration at Point 1 is 45 mg /L and the estimated nitrate concentration is
44.6 mg /L here. All other GeoTracker sites which exceed the MCL have nitrate concentrations that agree
with our estimated concentrations. Due to GeoTracker obfuscation, some of the sites are not accurately
located at the well site.
EXPLANATION
GeoTracker Site
With Nitrate Results Q Non- Detect
O < 22.5 mg /L
O > 22.5 mg /L but < 45 mg /L
© > 45 mg /L
F- I Groundwater Basin
Estimated Nitrate Concentration mg /L
< 22.5
#22.5 -36
l 36 - 45
I j45 -90
! >90
o 0 500 1,000
Feet i
O
A-21
Location 27 There are 12 CDPH supply wells at this location with a maximum nitrate concentration of 52 mg /L. The GeoTracker concentration and the estimated concentration agree at this location when viewed at a
larger scale.
EXPLANATION GeoTracker Site
With Nitrate Results o Non-Detect
Q < 22 5 mo/L
8 > 22.5 mg/L but < 45 mg!L
® > 45 mg!L
Groundwater Basin
Estimated Nitrate Concentration mg/L
<22.5
l ¡¡ 22.5-36
36-45
45-90 Err > 90
0 1,000 2,000 1
Feet
Langley Subarea Summary
Of the ten GeoTracker locations shown in the Langley Subarea with concentrations over the MCL (Figure A2), eight plot in an area we estimated the concentration to be above the MCL. There are two sites where the GeoTracker site reports a concentration greater than the MCL and the estimated concentration is shown as less than the MCL. At one location the maximum concentration in GeoTracker 45 mg /L. and the estimated concentration is 44.6 mg /L, At the other location the actual well location falls outside the groundwater basin boundary because the GeoTracker location is inaccurate due to obfuscation and clustering.
Appendix B -= Excluded Wells
Wells Excluded from Nitrate Mapping
We excluded 299 wells from the kriging dataset for estimation of nitrate concentrations for various reasons. We assumed the shallow aquifer extends to 400 feet deep, and we therefore excluded 54 wells
with known well depths greater than 400 feet. We assumed that any irrigation well with unknown depth had the potential to be greater than 400 feet deep, and therefore 195 irrigation wells were excluded.
Additionally, 27 domestic /irrigation wells with unknown depth were also excluded. Finally, 23
observation wells from regulated clean -up sites located in the urban, downtown Salinas area were
excluded from analysis due to extremely high nitrate values due to fertilizer and /or nitrate contamination.
Additionally, some data were excluded from our nitrate dataset. From selected wells, nitrate data from GeoTracker had less than qualifiers with unusually large nitrate values or had greater than qualifiers, i.e.
<16 mg /L; >63.9 mg /L. Instead of using the numerical given value, we excluded 12 points from our dataset. Eight of these points were from excluded wells from regulated clean -up sites mentioned above.
Table B3 summarizes these values.
Summary statistics for time -averaged nitrate concentrations from excluded wells are shown in Table B1.
The mean concentration was 41.1 mg /L. The median was 12.0 mg /L. Values ranged from 0.09 mg /L to 2,535 mg /L. 121 wells (19 %) had time -averaged concentrations over the MCL of 45 mg /L.
Figure B11 shows the excluded well locations and Table B2 lists the wells excluded.
Table Bi. Summary Statistics for Average Groundwater Nitrate Concentrations from Excluded Wells
Excluded Wells
Mean 69.9
Median 17,3
Standard Error 11.9
Minimum 0.09
Maximum 2,535
Number of wells 299
Number of wells (percentage) with concentrations over the MCL
103 (34 %)
1 The locations of CCGC member wells were obfuscated to protect member privacy. The locations of CCGC member
wells shown on Figure B1 were randomly adjusted up to 0.5 miles in both the east -west and north -south
directions. The wells are plotted within a 1 mil block centered over the actual well location.
B-1
ur4o'o izPpo'ow 12rVO'W
Ix
CARGLEY AREA
Excluded wells include wells with known well depth greater than 400 feet or well use that is either irrigation or demesticllrrigation with unknown well depth, and environmental monitoring wells In the Salinas area with possible nitrate or fertilizer contamination. See Table 82 for a complete list.
.itOSi
A.6 iO - R A E
SEASID AREA PAPO E
l,lskpl2
FOREEAYSUUAREA
^UPPER VALLEY WEAR
EXPLANATION
Excluded Wells
I or Di Well with Unknown o Depth
Environmental Monitoring Well with Possible Contamination
o Well Depth > 400 it
I= Groundwater Basin
o 0 6 10 15
111 I 11i1111 `xdoee
The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 ml' block centered over the actual well location.
1C06' betölrrie; U 018 SoOrtes: Esfl, U
°W INN
12114011W
Figure B1. Excluded Wells with Nitrate Data.
IPI'3P0'W
B-2
Tab
le B
Z.
Exc
lude
d W
ells
W
ell N
ame
Ave
rage
NO
3 W
ell
Dep
th
Use
S
ourc
e R
easo
n fo
r E
xclu
sion
. B
asin
AG
_BLA
IRS
19
.5
- 70
0 I
eNO
I W
ell
Dep
th >
400
F
oreb
ay
CC
GC
_005
7 70
.0
441
D
Hel
d V
isit
Wel
l D
epth
> 4
00
Pre
ssur
e
CC
GC
_014
1 6.
0 66
0 D
F
ield
Vis
it W
ell.
Dep
th >
400
E
ast
Sid
e
Wel
121_
irr
22.0
44
5 I
Fie
ld V
isit
Wel
l D
epth
>40
0 E
ast
Sid
e
CC
GC
_013
3 18
.0
460
D
Fie
ld V
isit
Wel
l Dep
th >
400
Pre
ssur
e
CC
GC
_010
9 1.
0 41
0 D
F
ield
Vis
it W
ell
Dep
th >
400
P
ress
ure
CC
GC
_014
4 2.
0 41
0 D
F
ield
Vis
it W
ell
Dep
th >
400
F
oreb
ay
CC
GC
_004
5 4.
0 57
0 D
/I F
eld
Vis
it W
ell
Dep
th >
400
Pre
ssur
e
CC
GC
_004
7 0S
58
0 D
F
eld
Vis
it W
ell
Dep
th>
400
Pre
ssur
e
CC
GC
_004
8 2.
0.
670
D/I
Fie
ld V
isit
Wel
l D
epth
>40
0 P
ress
ure
CC
GC
_044
4 O
5 44
6 D
/I F
ield
Vis
it W
ell D
epth
>40
0 P
ress
ure
CC
GC
_044
2 1.
0 53
0 D
P
Fel
d V
isit
Wel
l D
epth
>40
0 P
ress
ure
CC
GC
0058
0.
5 41
6 D
F
ield
Vis
it W
ell
Dep
th >
400
P
ress
ure
CC
GC
_006
9 0.
9 59
5 D
P
Fie
ld V
isit
Wel
l D
epth
> 4
00
Pre
ssur
e
CC
GC
_007
1 2.
0 51
2 0/
I F
ield
Vis
it W
ell
Dep
th >
400
Pre
ssur
e
CC
GC
_004
0 50
.0
544
D/I
Fie
ld V
isit
Wel
l D
epth
>40
0 F
oreb
ay
CC
GC
_004
2 10
.0
410
0/1
Fie
ld V
isit
Wel
l D
epth
>40
0 F
oreb
ay
CC
GC
_013
8 69
0.0
640
I F
ield
Vis
it W
ell
Dep
th >
400
E
ast
Sid
e
CC
GC
_003
1 3.
0 70
0 0/
I F
ield
Vis
it W
ell
Dep
th >
400
P
ress
ure
CC
GC
_003
2 17
4.0
700
0/1
Fie
ld V
isit
Wel
l D
epth
>40
0 P
ress
ure
CC
GC
0034
17
.0
600
D/I
Fie
ld V
isit
Wel
l D
epth
> 4
00
Eas
t S
ide
CC
GC
_003
6 2.
0 -
600
D
Fie
ld V
isit
Wel
l D
epth
>40
0 P
ress
ure
CC
GC
_003
8 3.
0 58
0 D
/I F
ield
Vis
it W
ell
Dep
th >
400
P
ress
ure
CC
GC
_040
3 98
.0
608
D/I
Fie
ld V
isit
Wel
l D
epth
>40
0 E
ast
Sid
e
CC
GC
_013
9 19
1.0
472
D/I
Fie
ld V
isit
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l Dep
th >
400
Eas
t S
ide
CC
GC
_012
7 2.
0 78
0 D
/I F
ield
Vis
it W
ell
Dep
th >
400
Pre
ssur
e
CC
GC
_012
8 2.
0 78
0 D
/I F
ield
Vis
it W
ell
Dep
th >
400
Pre
ssur
e
CC
GC
0126
1.
0 10
10
D/I
Fie
ld V
isit
Wel
l D
epth
> 4
00
Pre
ssur
e
CC
GC
_000
7 82
.7
460
D/I
Fie
ld V
isit;
eN
O1
Wel
l D
epth
>40
0 E
ast S
ide
CC
GC
0136
10
.2
589
D
Fie
ld V
isit;
US
GS
-GA
P
Wel
l D
epth
>40
0 P
ress
ure
Fie
ld V
isit;
US
GS
-NW
IS;
US
GS
-
CC
GC
_014
0 4.
7 66
0 D
G
AP
W
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> 4
00
Eas
t Sid
e
San
lera
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deep
PW
10
25
440
Unk
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NL
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0 E
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3619
1012
1184
801
1.2
410
D
US
GS
-GA
P
Wel
l Dep
th >
400
F
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ay
3619
4112
1153
701
0.9
670
D
US
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F
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3643
3712
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6 45
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U
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3635
5212
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64.0
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US
GS
-NW
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l Dep
th >
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Eas
t S
ide
3641
1112
1410
701
62.7
43
0 I
US
GS
-NW
IS
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l Dep
th >
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P
ress
ure
3647
5712
1373
301
0.1
472
Unk
now
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Lang
ley
3619
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1160
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8.
2 88
3 U
nkno
wn
US
GS
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GA
MA
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th >
400
For
ebay
36
2800
1212
2000
1 4.
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; G
AM
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36
3618
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8190
1 8.
4 49
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nkno
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GA
MA
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Pre
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Wel
t N
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NO
3 W
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U
se
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rce
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son
for
Exc
lusi
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in
3639
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51.5
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4 U
nkno
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MA
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th >
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3641
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SG
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; G
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epth
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ide
3641
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17.1
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nkno
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WIS
; G
AM
A
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l D
epth
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00
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t S
ide
3642
1712
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3.6
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U
SG
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E
ast
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4217
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2 4.
2 61
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bs
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WIS
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epth
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ide
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6.1
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U
SG
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IS;
GA
MA
W
ell
Dep
th >
400
E
ast
Sid
e 36
4357
1213
7570
1 31
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619
Unk
now
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SG
S -N
WIS
; G
AM
A
Wel
l D
epth
> 4
00
Eas
t S
ide
3645
0012
1480
001
0.1
1364
U
nkno
wn
US
GS
-NW
IS;
GA
MA
W
ell
Dep
th >
400
P
ress
ure
3646
0012
1430
001
3.0
640
Unk
now
n U
SG
S -N
WIS
; G
AM
A
Wel
l D
epth
> 4
00
Pre
ssur
e 36
4800
1213
7000
1 6.
7 50
0 U
nkno
wn
US
GS
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IS;
GA
MA
W
ell
Dep
th >
400
La
ngle
y 36
3507
1213
8060
1 81
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700
D
US
GS
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IS;
US
GS
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P
Wel
l D
epth
> 4
00
Pre
ssur
e 36
3718
1213
0200
1 22
0.0
700
D
US
GS
-NW
IS;
US
GS
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P
Wel
l D
epth
> 4
00
Eas
t S
ide
3641
1712
1411
401
44.2
50
0 D
U
SG
S -N
WIS
; U
SG
S -G
AP
W
ell
Dep
th >
400
P
ress
ure
AG
WE
LL (
1)
19.9
I
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
Dep
th
For
ebay
A
G W
ELL
(12
) 24
.6
I eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
For
ebay
A
G W
ELL
(13
) 6.
2 1
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
Dep
th
For
ebay
A
G W
ELL
(14
) 12
.6
I eN
01
Irrig
atio
n w
ell
with
Unk
now
n W
ell
Dep
th
For
ebay
A
G W
ELL
(15
) 51
.8
I eN
OI
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
Upp
er V
alle
y A
G W
ELL
(2)
13
.7
I eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
For
ebay
A
G W
ELL
(3)
26
.6
I eN
OI
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
For
ebay
A
G W
ELL
(4)
45
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I eN
O!
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
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F
oreb
ay
AG
WE
LL (
5)
276.
6 I
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
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th
For
ebay
A
G W
ELL
(6)
59
.6
I eN
01
Irrig
atio
n w
ell
with
Unk
now
n W
ell
Dep
th
For
ebay
A
G W
ELL
(8)
9.
1 I
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
Dep
th
For
ebay
A
G W
ELL
(9)
7.
3 I
eN01
Ir
rigat
ion
wel
l with
Unk
now
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ell
Dep
th
Upp
er V
alle
y N
EW
AG
20
.8
I eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
F
oreb
ay
OLD
AG
19
7.1
I eN
01
Irrig
atio
n w
ell
with
Unk
now
n W
ell
Dep
th
For
ebay
1
144.
7 I
eN01
Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
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E
ast
Sid
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W
3.5
eN01
Ir
rigat
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wel
l w
ith U
nkno
wn
Wel
l D
epth
P
ress
ure
AW
1 (1
) 2.
4 eN
01
Irrig
atio
n w
ell
with
Unk
now
n W
ell
Dep
th
Pre
ssur
e A
W 1
(2
) 5.
5 eN
01
Irrig
atio
n w
ell
with
Unk
now
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ell
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th
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W 1
(3
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0 eN
01
Irrig
atio
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with
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now
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th
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ssur
e A
W 2
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4 eN
01
Irrig
atio
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ell
with
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now
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ell
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th
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W 2
(2
) 2.
7 eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
P
ress
ure
AW
2 (3
) 15
.2
eN01
Ir
rigat
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wel
l with
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now
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ell
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th
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ssur
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W 3
4.
1 eN
OI
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
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P
ress
ure
AG
_WE
LL_S
U
16.3
eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
P
ress
ure
WE
LL 1
15
63
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
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th
Eas
t S
ide
WE
LL 2
48
.0
eN01
Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
l Dep
th
Eas
t S
ide
LON
014
01
69.0
eN
OI
Irrig
atio
n w
ell
with
Unk
now
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ell
Dep
th
Upp
er V
alle
y LO
N01
4 02
19
9.0
eNO
I Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
l Dep
th
Upp
er V
alle
y LO
N01
4 R
ES
95
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eN01
Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
l Dep
th
Upp
er V
alle
y A
G_W
ELL
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22
6.1
eNO
I Ir
rigat
ion
wel
l with
Unk
now
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ell D
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E
ast
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B-4
Wei
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ame
Ave
rage
NO
3 W
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th
Use
So
urce
R
easo
n fo
r E
xclu
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B
asin
SIP
1
2.5
eN01
Ir
rigat
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wel
l w
ith U
nkno
wn
Wel
l Dep
th
Pre
ssur
e
AB
RA
MS
9.
7 eN
OI
Irrig
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ell
with
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now
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ell D
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P
ress
ure
ALT
UR
AS
0.
4 eN
01
Irrig
atio
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ell
with
Unk
now
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F
oreb
ay
BIN
SA
CC
A
13.7
eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
For
ebay
CA
YM
US
7.
5 eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l Dep
th
Pre
ssur
e
RIV
ER
1
452
eNO
I Ir
rigat
ion
wel
l with
Unk
now
n W
ell D
epth
P
ress
ure
AG
44
.1
eN01
Ir
rigat
ion
wel
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Unk
now
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epth
F
oreb
ay
WE
LL #
1 E
LEC
TR
I 15
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eN01
Ir
rigat
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wel
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now
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ell D
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U
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Val
ley
FC
N
OR
TH
14
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eN01
Ir
rigat
ion
wel
l with
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now
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ell
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th
For
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FC
SO
UT
H
92.0
eN
01
Irrig
atio
n w
ell
with
Unk
now
n W
ell
Dep
th
For
ebay
WE
LL N
18
7.8
eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
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th
For
ebay
AG
W
ELL
C
2.
0 eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
P
ress
ure
AG
_WE
LL_F
S
215.
1 eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
E
ast
Sid
e
AG
_WE
LL
PR
5.
9 eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
E
ast
Sid
e
AG
WE
LL (
3)
13.5
eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
P
ress
ure
ALI
SA
L 2
76.2
eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
F
oreb
ay
ALI
SA
L 3
70.9
eN
01
Irrig
atio
n w
ell w
ith U
nkno
wn
Wel
l D
epth
F
oreb
ay
WE
LL (
1)
134.
6 eN
01
Irrig
atio
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ell
with
Unk
now
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ell
Dep
th
Eas
t S
ide
WE
LL (
2)
27.0
eN
01
Irrig
atio
n w
ell
with
Unk
now
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ell
Dep
th
Eas
t S
ide
WE
LL (
3)
0.2
eN01
Ir
rigat
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wel
l w
ith U
nkno
wn
Wel
l D
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La
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y
LA R
EIN
A
20.7
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OI
Irrig
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ell
with
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now
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th
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AIN
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19.8
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01
Irrig
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wn
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oreb
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ER
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13
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eN01
Ir
rigat
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now
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ell
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th
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AG
WE
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10
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eN01
Ir
rigat
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wel
l with
Unk
now
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P
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WE
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0.
4 eN
01
Irrig
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Wel
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th
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e
AG
WE
LL 1
(3)
82
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eNO
I Ir
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wel
l with
Unk
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P
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AG
WE
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(4)
9.
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OI
Irrig
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th
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e
AG
WE
LL 1
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10
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eN01
Ir
rigat
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wel
l with
Unk
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P
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AG
WE
LL 1
(6
) 15
4.1
eN01
Ir
rigat
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wel
l with
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ast
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AG
WE
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(1
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01
Irrig
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ast
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AG
WE
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I Ir
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wel
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AG
WE
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0 eN
01
Irrig
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Wel
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th
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e
AG
WE
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8 eN
01
Irrig
atio
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wn
Wel
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th
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e
AG
WE
LL 2
(5
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7 eN
01
Irrig
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ith U
nkno
wn
Wel
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th
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e
AG
WE
LL 3
71
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eN01
Ir
rigat
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wel
l with
Unk
now
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ell D
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E
ast
Sid
e
AG
WE
LL 5
54
.0
eN01
Ir
rigat
ion
wel
l with
Unk
now
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ell
Dep
th
Eas
t S
ide
WE
LL
99.9
eN
01
Irrig
atio
n w
ell
with
Unk
now
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ell
Dep
th
For
ebay
WE
LL 2
22
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eN01
Ir
rigat
ion
wel
l with
Unk
now
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ell
Dep
th
For
ebay
AG
_AM
AR
AL
11.4
eN
01
Irrig
atio
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ell
with
Unk
now
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th
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AG
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LL55
B
22.5
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01
Irrig
atio
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ell
with
Unk
now
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th
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e
AG
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LL95
A
23.8
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01
Irrig
atio
n w
ell
with
Unk
now
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ell
Dep
th
Pre
ssur
e
AG
_WE
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N
2.4
eN01
Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
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E
ast
Sid
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WE
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12.6
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01
Irrig
atio
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with
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now
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th
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alle
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B-5
Wel
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Wel
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Use
S
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xclu
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A
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18
0.0
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01
Irrig
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wn
Wel
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ast
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10
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I eN
01
Irrig
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wn
Wel
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2
65.2
I
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Ir
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wel
l with
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OM
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32
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I eN
01
Irrig
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OM
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14
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I eN
Ol
Irrig
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60
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01
Irrig
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with
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JOH
NS
ON
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2
28.8
I
eN01
Ir
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wel
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wn
Wel
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F
oreb
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JOH
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D
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40
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I eN
01
Irrig
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oreb
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LOS
CO
CH
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1
148.
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Ir
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16
4.0
I eN
01
Irrig
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A
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eNO
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wel
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KY
RC
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70
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I eN
01
Irrig
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Wel
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ZA
BA
LA A
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11
1.5
i eN
01
Irrig
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ell
with
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Z
AB
ALA
AW
2
10.5
I
eNO
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wel
l with
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For
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Z
AB
ALA
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3
216.
0 eN
01
Irrig
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wn
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oreb
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AG
WE
LL
158.
0 eN
01
Irrig
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nkno
wn
Wel
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Eas
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ide
WE
LL
1.3
eN01
Ir
rigat
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wel
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wn
Wel
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th
For
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W
ELL
5
6.4
eN01
Ir
rigat
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wel
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For
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W
ELL
#1
104.
0 eN
OI
Irrig
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141
) 14
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Ir
rigat
ion
wel
l with
Unk
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ress
ure
WE
LL 1
(2)
16
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eN01
Ir
rigat
ion
wel
l with
Unk
now
n W
ell
Dep
th
Pre
ssur
e W
ELL
1 (
3)
16.8
eN
01
Irrig
atio
n w
ell
with
Unk
now
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ell
Dep
th
Pre
ssur
e W
ELL
2
3.3
eN01
Ir
rigat
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wel
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ith U
nkno
wn
Wel
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epth
P
ress
ure
AIR
PO
RT
WE
LL 7
12
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eN01
Ir
rigat
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wel
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nkno
wn
Wel
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ley
ALA
NS
VIN
E W
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12
7.0
eN01
Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
l D
epth
U
pper
Val
ley
ALT
A L
OM
A 7
12
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eN01
Ir
rigat
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wel
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ell
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Upp
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alle
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RR
OY
O L
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A 7
12
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l Ir
rigat
ion
wel
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nkno
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Wel
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U
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Val
ley
CA
RM
EL
MA
IN
8.2
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I Ir
rigat
ion
wel
l w
ith U
nkno
wn
Wel
l D
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F
oreb
ay
CA
SA
GR
AN
DE
MA
I 27
.6
eN01
Ir
rigat
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wel
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Ir
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atio
n
CC
GC
_011
5 17
2.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_011
6 17
4.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_004
1 28
.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_006
1 23
7.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_049
6 23
.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_015
9 9.
0 D
/I F
ield
Vis
it D
omes
tic /Ir
rigat
ion
CC
GC
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4 78
.0
D/I
Fie
ld V
isit
Dom
estic
/Irrig
atio
n
CC
GC
_017
3 16
6.0
D/I
Fie
ld V
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estic
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igat
ion
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GC
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D/I
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ld V
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n
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ld V
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n
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3 5.
0 D
/I F
ield
Vis
it D
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tic /Ir
rigat
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CC
GC
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6 12
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D/I
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ld V
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Dom
estic
/Irrig
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n
CC
GC
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6 16
2.0
D/I
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ld V
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estic
/Irr
igat
ion
AG
DO
M
53.3
D
/I P
rovi
ded
Lab
Dat
a; e
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tic /I
rrig
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n M
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n wel
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Bas
in
For
ebay
For
ebay
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Eas
t S
ide
Eas
t S
ide
For
ebay
For
ebay
E
ast
Sid
e
Pre
ssur
e
For
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F
oreb
ay
For
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For
ebay
P
ress
ure
Pre
ssur
e
For
ebay
For
ebay
P
ress
ure
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e P
ress
ure
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Pre
ssur
e
Tab
le B
3. S
ampl
ed d
ata
poin
ts e
xclu
ded
due
to la
rge
less
tha
n or
gre
ater
than
qua
lifie
r.
Wel
l N
ame
Bas
in
Wel
l Dep
th
Sam
ple
Dat
e C
onst
ituen
t Q
ualif
ier
Res
ult.
Uni
ts
Use
S
ourc
e
2701
675
-001
U
pper
Val
ley
6/20
/200
2 N
O3
<
10
MG
/L
Unk
now
n G
AM
A
2702
444
001
Pre
ssur
e 5/
23/2
005
NO
3 <
16
M
G /L
U
nkno
wn
GA
MA
M
W-3
(18
) E
ast
Sid
e 2/
2/20
06
NO
3 >
67
.31
MG
/L
Obs
erva
tion
GA
MA
MW
-6 (
13)
Eas
t S
ide
2/2 /
2006
N
O3
>
61.1
1 M
G /L
O
bser
vatio
n G
AM
A
OW
-1
Pre
ssur
e 80
10
/3/2
007
NO
3 >
49
.5
MG
/L
Obs
erva
tion
GA
MA
OW
-1
Pre
ssur
e 80
4/
1/20
09
NO
3 >
67
.05
MG
/L
Obs
erva
tion
GA
MA
OW
-2
Pre
ssur
e 80
10
/3/2
007
NO
3 >
52
2 M
G /L
O
bser
vatio
n G
AM
A
OW
-2
Pre
ssur
e 80
4/
1/20
09
NO
3 >
54
0 M
G /L
O
bser
vatio
n G
AM
A
OW
-4
Pre
ssur
e 84
10
/3/2
007
NO
3 >
63
.9
MG
/L
Obs
erva
tion
GA
MA
O
W-4
P
ress
ure
84
4/1/
2009
N
O3
>
61.2
M
G /L
O
bser
vatio
n G
AM
A
OW
-5
Pre
ssur
e 82
10
/3/2
007
NO
3 >
43
2.45
M
G /L
O
bser
vatio
n G
AM
A
OW
-5
Pre
ssur
e 82
4/
1/20
09
NO
3 >
10
12.5
M
G /L
O
bser
vatio
n G
AM
A
B-1
0
Appendix C - Quality Assurance and
Quality Control
Held Blanks
Field blanks detect possible constituent sources contributed from sampling methods and equipment.
Examples include, but are not limited to, improperly cleaned sampling equipment, persistent airborne
constituents in the sampling environment, and constituent sources in the sample containers. Fourteen
field blanks were collected.2
Potassium, alkalinity, calcium, sodium, nitrate as NO3, nitrate as N, nitrate + nitrite as N, nitrite as N,
bicarbonate, and sulfate were detected in the field blanks. Detected concentrations were less than or
equal to the PQL in 11 samples and above the PQL in three samples. Calcium was detected at a
concentration of 2 mg /L in one field blank, which is above the PQL of 1 mg /L. NO3 +NO2 as N was
detected at concentrations of 0.2 and 0.3 mg /L, which are both above the PQL of 0.1 mg /L. NO3 as N
was detected at a concentration of 0.2 mg /L, which is above the PQL of 0.1 mg /L.
The table below summarizes detected values of nitrate species in the field blanks. Only three detected
concentrations exceed the PQL.
2 Field blanks were collected by pumping deionized water through a length of clean tubing. Sample
bottles were filled, preserved, stored, and transported using the same procedures as used for the well
water samples.
C-1
Table Cl. Concentrations of NO3, NO3 as N, NO3 +NO2 as N, and NO2 as N in the field blanks. NO3 NO3 as N NO3+NO2 as N NO2 as N Sample ID Date
(mg/L) (mg/L) (mg/L) (rng/L) PQL 1 0.1 0.1 0.1
CCGC_0035 10/21/2013 ND ND ND ND CCGC_0043 10/22/2013 ND ND ND ND CCGC_0055 10/23/2013 ND ND ND ND CCGC_0028 10/24/2013 ND ND ND ND CCGC_0013 10/25/2013 ND ND ND ND CCGC_0107 3/10/2014 ND ND 0.1 ND CCGC_0158 3/11/2014 ND ND ND ND CCG C__0121 3/12/2014 ND ND 0.1 ND CCGC_0169 3/13/2014 ND ND 0.1 0.1 CCGC_0136 3/14/2014 ND ND 0.1 0.1 CCGC_0194 3/19/2014 ND ND `!,2. ND Penny_Irr 7/15/2014 ND ND ND ND Cla usen_D 7/17/2014 ND ND ND ND CCGC_0178 8/27/2014 1 0.2 ::','z ND
Field Duplicates
Duplicates monitor matrix consistency or heterogeneity. Fourteen field duplicates were collected. Most duplicate sample results (99 percent) agreed, had differences within 10- percent, or had differences within the PQL (Practical Quantitation Limit) of the constituents analyzed. Of the remaining sample duplicate results, variations could be attributed to lab analytical variability or constituent sources introduced in the laboratory, field, or sampling equipment. The following table lists the sample duplicates and the percent differences for nitrate species. The differences in NO2 as N concentrations for the RIVERR1 sample and duplicate exceed 10- percent, but have differences within the PQL of 0.1 mg /L. All other nitrate species concentration differences were less than 10- percent.
Table C. Sample and duplicate NO3, NO3 as N, NO3 +NO2 as N, and NO2 as N concentrations and percent differences.
Sample ID Date NO3
(mg /L) NO3asN
(mg /L) NO3 +NO2asN
(mg /L) NO2asN (mg /L)
CCGC_0035 10/21/2013 65 14.6 15 0.4 CCGC_0035 10/21/2013 65 14.6 15 0.4
Percent Difference 0.0% 0.0% 0.0% 0.0% CCGC_0043 10/22/2013 142 32.1 32.4 0.3 CCGC_0043 10/22/2013 145 32.7 33 0.3 Percent Difference 2.1:% 1.9% 1.8% 0.0% CCGC_0045 10/23/2013 4 0.8 1.1 0.3 CCGC_0045 10/23/2013 4 0.8 1.1 0.3 Percent Difference 0.0% 0.0% 0.0% 0.0% CCGC_0028 10/24/2013 106 23.9 24.2 0.3 CCGC_0028 10/24/2013 106 24 24.4 0.3 Percent Difference 0.0% 0.4% 0.8% 0.0%
C-2
Sample ID Date
NO3
(mg/L) NO3 as N
(mg/L) NO3+NO2 as N
(mg /L)
NO2 as N
(mg/L)
CCGC_0013 10/25/2013
CCG C_0013 10/25/2013
2
2
0.5
0.5
0.8
0.8
0.3
0.3
Percent Difference 0.0% 0.0% 0.0% 0.0%
CCGC_0107 3/10/2014
CCGC_0107 3/10/2014
486
486
110
110
110
110
ND
ND
Percent Difference 0.0% 0.0% 0.0% 0.0%
CCGC_0158 3/11/2014
CCGC_0158 3/11/2014
62
63
14.1
14.1
14.3
14.4
0.2
0.2
Percent Difference 1.6% 0.0% 0.7% 0.0%
CCGC_0121 3/12/2014
CCGC_0121 3/12/2014
209
214
47.2
48.3
47.3
48.4
0.1
0.1
Percent Difference 2.4% 2.3% 2.3% 0.0%
CCGC_0169 3/13/2014
CCG C_0169 3/13/2014
20
20
4.6
4.6
5
5
0.4
0.4
Percent Difference 0.0% 0.0% 0.0% 0.0%
CCGC_0136 3/14/2014
CCGC_0136 3/14/2014
10
10
2.3
2.3
2.6
2.6
0.4
0.3
Percent Difference 0.0% 0.0% 0.0% 28.6%
CCGC_0194 3/19/2014
CCGC_0194 3/19/2014
454
454
100.5
100.8
102.6
102.5
ND
ND
Percent Difference 0.0% 0.3% 0.1% 0.0%
Penny_Irr 7/15/2014 6 1.3 1.6 0.3
Penny_Irr 7/15/2014 6 1.3 1.6 0.3
Percent Difference 0.0% 0.0% 0.0% 0.0%
Clausen_D 7/17/2014
Clausen_D 7/17/2014
25
25
5.6
5.6
5.9
5.9
0.3
0.3
Percent Difference 0.0% 0.0% 0.0% 0.0%
CCGC_0178 8/27/2014
CCGC_0178 8/27/2014
45
45
10.2
10.2
10.6
10.6
0.4
0.4
Percent Difference 0.0% 0.0% 0.0% 0.0%
Anion-Cation Charge Balance
Anion -cation charge balance was calculated using concentrations of the major anions and cations in
milliequivalents per liter (meq /L). The difference between the two sums was calculated as a percentage:
Anions - Cations x 100
Anions + Cations
We use +/- 5 percent as a guide for an acceptable percent difference. The cation /anion balance difference
exceeded 5 percent for 66 of 247 samples (27 %). The results are summarized in the following table. We
have inquired with the laboratory to look into samples that exceed 10 percent. We are awaiting the
laboratory's response.
C-3
Table C3. Sum cations and anions and cation /anion balance.
Sample ID Date Sum Cations
(meq /L) Sum Anions
(meq /L) Anion /Cation balance
(% difference) Use Basin CCGC_0005 10/21/2013 12.43 12.19 1.0% D East Side CCGC_0007 10/21/2013 6.61 6.47 1.1% D/I East Side CCGC_0009 10/21/2013 509 5,72 1.4% D East Side CCGC_0010 10/21/2013 2600 25.24 15% D Pressure CCGC_0012 10/21/2013 9.85 9.73 0.6% D Pressure CCGC_0017 10/21/2013 22.78 21.90 2.0% D East Side CCGC_0018 10/21/2013 11.71 11.55 0.7% D East Side CCGC_0020 10/21/2013 10.96 10.75 1.0% D Pressure CCGC_0023 10/21/2013 7.30 7.34 -0.2% D/I Pressure CCGC_0035 10/21/2013 19.24 18.59 1.7% D Pressure CCGC_0035 10/21/2013 19.16 18.57 15% D Pressure CCGC_0054 10/21/2013 22.67 21.75 2.1% D Pressure CCGC_0060 10/21/2013 6.77 6.61 1.2% D Pressure CCGC_0069 10/21/2013 12.47 12.17 1.2% D/I Pressure CCGC_0070 10)21/2013 10.95 10.93 0.1% D Pressure CCGC_0004 10/22/2013 7.29 6.83 3.2% D East Side CCGC_0008 10/22/2013 21.71 19,53 5.3% D Forebay CCGC_0016 10/22/2013 11.44 10.97 2.1% D Upper Valley CCGC_0031 10/22/2013 17.49 16.31 3.5% D/I Pressure CCGC_0033 10/22/2013 11.79 11.09 3.1% D East Side CCGC_0034 10/22/2013 8.24 7.85 2.5% D/I East Side CCGC_0036 10/22/2013 7.79 7.44 2.3% D Pressure CCGC_0037 10/22/2013 30.89 29.71 1.9% D Pressure CCGC_0038 10/22/2013 8.12 8.00 0.8% D/I Pressure CCGC_0043 10/22/2013 18.25 16,39 5.4% Dui Forebay CCGC_0043 10/22/2013 17.99 16,58 4.1% D/I Forebay CCGC_0044 10/22/2013 39.91 37.11 3.6% D/I Forebay CCGC_0064 10/22/2013 5.51 5.30 - 2.0% D/I Forebay CCGC_0065 10/22)2013 26.60 24.75 3.6% D/I Upper Valley CCGC_0066 10/22/2013 11.96 11.34 2.6% D/I Upper Valley CCGC_0068 10/22/2013 20.40 19.45 2.4% D Pressure CCGC_0014 10/23/2013 19.71 18.01 4.5% D Forebay CCGC_0045 10/23/2013 6.49 5.92 4.6% D/I Pressure CCGC_0045 10/23/2013 6.49 5.94 4.4% D/I Pressure CCGC_0046 10/23/2013 6.49 6.00 3.9% D Pressure CCGC_0047 10/23/2013 6.74 6.36 2.9% D Pressure CCGC_0048 10/23/2013 7.55 7.07 3.3% D/I Pressure CCGC_0049 10/23/2013 15.43 14.19 4.2% D/I Forebay CCGC_0052 10/23/2013 19.71 18.60 2.9% D Forebay CCGC_0053 10/23/2013 54.86 50.65 4.0% D Forebay CCGC_0055 10/23/2013 22.23 20.23 4.7% D East Side CCGC_0056 10/23/2013 20.60 18.73 4.7% D Pressure CCGC_0057 10/23/2013 14,42 13.43 30% D Pressure CCGC_0059 10/23/2013 14.13 12.96 4.3% D Pressure CCGC_0061 10/23/2013 23.94 22.51 3.1% D/I Forebay CCGC_0062 10/23/2013 5,26 4.86 4.0% D Upper Valley CCGC_0063 10/23/2013 18.88 17.38 4.2% D Forebay CCGC_0072 10/23/2013 4.28 4.11 2,0% D/I Forebay CCGC_0074 10/23/2013 16.31 15.16 3.7% D/I Forebay CCGC 0075 10/23/2013 18.93 17.49 4,0% D/I Forebay CCGC_0001 10/24/2013 11.97 10.74 5.4% D Pressure CCGC_0002 10/24/2013 16.55 15.00 4.9% D Forebay
C -4
Sample ID Date
Sum Cations
(meq /L) Sum Anions
(meq /L) Anion /Cation balance
(% difference) Use Basin
CCGC_0003 10/24/2013 25.12 22.54 5.4% D Forebay
CCGC_0019 10/24/2013 6.15 5.74 3.5% D Forebay
CCGC_0024 10/24/2013 6.07 5.60 4.0% D Forebay
CCGC_0025 10/24/2013 9.62 8.82 4.3% D Forebay
CCGC_0026 10/24/2013 5.18 4.77 4.2% D Forebay
CCGC_0027 10/24/2013 8.45 7.86 3.6% D» Forebay
CCGC_0028 10/24/2013 10.29 9.45 4.2% D Forebay
CCGC_0028 10/24/2013 10.34 9.42 4.6% D Forebay
CCGC_0029 10/24/2013 4.67 4.29 4.2% D Forebay
CCGC_0030 10/24/2013 4.00 3.71 3.7% D Forebay
CCGC_0040 10/24/2013 12.61 11.42 5.0% D/I Forebay
CCGC_0041 10/24/2013 8.31 7.62 4.3% D/I Forebay
CCGC_0042 10/24/2013 5.27 4.98 2.9% D/I Forebay
CCGC_0050 10/24/2013 7.47 8.02 -3.5% D/I Forebay
CCGC_0051 10/24/2013 4.91 4.71 2.1% D Forebay
CCGC_0006 10/25/2013 17.62 15.95 5.0% D Forebay
CCGC_0011 10/25/2013 9.58 8.84 4.0% D Forebay
CCGC_0013 10/25/2013 10.49 9.73 3.7% D Upper Valley
CCGC_0013 10/25/2013 10.53 9.71 4.1% D Upper Valley
CCGC_0015 10/25/2013 30.11 27.32 4.9% D Forebay
CCGC_0021 10/25/2013 7.03 6.53 3.7% D/I East Side
CCGC_0022 10/25/2013 27.17 24.73 4.7% I East Side
CCGC_0032 10/25/2013 25.11 23.01 4.4% D/I Pressure
CCGC_0039 10/25/2013 10.32 9.41 4.6% D Pressure
CCGC_0058 10/25/2013 8.05 7.55 3.2% D Upper Valley
CCGC_0067 10/25/2013 8.06 7.43 4.1% D Forebay
CCGC_0071 10/25/2013 6.16 5.61 4.7% D/I Pressure
CCGC_0073 10/25/2013 4.98 4.90 0.9% D/I Forebay
Well21_Irr 1/10/2014 6.46 6.66 -1.5% I East Side
0489_D/I 1/22/2014 2.42 2.50 -1.6% D/I Langley
Penny_Irr 1/23/2014 6.41 6.76 -2.6% I East Side
Clausenl_ 1/23/2014 5.72 6.04 -2.8% I Upper Valley
Clausen_D 1/23/2014 6.33 6.77 -3.4% D Upper Valley
CCGC_0109 3/10/2014 5.11 5.04 0.7% D Pressure
CCGC_0146 3/10/2014 10.82 10.15 3.2% D Pressure
CCGC_0142 3/10/2014 16.94 15.65 3.9% D Forebay
CCGC_0143 3/10 /2014 8.82 8.04 4.7% D Forebay
CCGC_0144 3/10/2014 12.38 11.86 2.1% D Forebay
CCGC_0145 3/10/2014 9.90 9.50 2.1% D Pressure
CCGC_0107 3/10/2014 23.84 22.55 2.8% D East Side
CCGC_0107 3/10/2014 23.80 21.00 6.3% D East Side
CCGC_0112 3/10/2014 18.18 16.60 4.5% D Pressure
CCGC_0111 3/10/2014 9.06 8.74 1.8% D Pressure
CCGC_0110 3/10/2014 20.41 18.83 4.0% D/I Pressure
CCGC_0150 3/11/2014 7.86 6.76 7.6% D Forebay
CCGC_0113 3/11/2014 14.67 14.12 1.9% D/I Pressure
CCGC_0118 3/11/2014 18.27 15.64 7.7% D Pressure
CCGC_0155 3/11/2014 12.83 11.19 6.8% D Forebay
CCGC_0163 3/11/2014 61.01 53.98 6.1% D Upper Valley
CCGC_0152 3/11/2014 8.34 7.42 5.9% D Forebay
CCGC_0153 3/11/2014 60.58 52.11 7.5% D Upper Valley
CCGC_0162 3/11/2014 8.88 7.94 5.6% D Forebay
CCGC_0164 3/11/2014 19.64 17.32 6.3% D Forebay
C-5
Sample ID Date Sum Cations
(meq /L) Sum Anions
(meq /L)
Anion /Cation balance (% difference) Use Basin
CCGC_0157 3/11/2014 21.83 18.93 7.1% D Forebay CCGC_0158 3/11/2014 16.01 14.00 6.7% D Forebay CCGC_0158 3/11/2014 16.00 14.06 6.4% D Forebay CCGC_0156 3/11/2014 21.28 18.09 8.1% D Forebay CCGC_0114 3/11/2014 14.85 13.96 3.1% D Pressure CCGC_0115 3/11/2014 11.52 10.16 6.3% D/I East Side CCGC_0116 3/11/2014 11.48 10.21 5.9% D/I East Side CCGC_0117 3/11/2014 7.42 6.56 6.2% D/I Pressure CCGC_0120 3/11/2014 15.57 13.52 7.1% D/I Pressure CCGC_0178 3/12/2014 8.97 7.69 7.7% D East Side CCGC_0121 3/12/2014 14.31 12.43 7.0% D East Side CCGC_0121 3/12/2014 14.36 12,66 6.3% D East Side CCGC_0165 3/12/2014 17.88 15.78 6.2% D Forebay CCGC_0159 3/12/2014 6.45 5.68 6.4% D/I Pressure CCGC_0161 3/12/2014 9.82 8.95 4.7% D Forebay CCGC_0160 3/12/2014 10.44 9.20 6.3% D Forebay CCGC_0127 3/12/2014 5.67 4.92 7.1% D/I Pressure CCGC_0128 3/12/2014 5.50 4.69 7.9% D/I Pressure CCGC_0126 3/12/2014 5.48 4.78 6.8% D/I Pressure CCGC_0122 3/12/2014 19.44 17.25 6.0% D Pressure CCGC_0125 3/12/2014 10.56 8.99 8.0% D East Side CCGC_0179 3/12/2014 18.71 16,25 7.0% D/I Forebay CCGC_0180 3/12/2014 7.75 6,71 7.1% D Upper Valley CCGC_0181 3/12/2014 8.35 7.32 6.6% D Upper Valley CCGC_0123 3/12/2014 28.51 24.65 7.3% D Pressure CCGC_0129 3/12/2014 8.71 7.65 6.5% D Langley CCGC_0151 3/12/2014 9,46 8,40 5.9% D Forebay CCGC_0124 3/12/2014 11.41 9.96 6.8% D East Side CCGC_0135 3/13/2014 9,42 8.65 4.2% D Pressure CCGC_0134 3/13/2014 14.23 12.65 5.9% D Pressure CCGC_0133 3/13/2014 8.71 8,27 2.6% D Pressure CCGC_0184 3/13/2014 8.34 7.31 6.6% D Pressure CCGC_0185 3/13/2014 10.84 9.60 6.1% D Pressure CCGC_0182 3/13/2014 5.43 4.55 8.8% D/I Pressure CCGC_0168 3/13/2014 11.53 10.31 5.6% D Upper Valley CCGC_0166 3/13/2014 6.41 5,96 3.7% D Upper Valley CCGC_0170 3/13/2014 43.91 38,48 6.6% D Upper Valley CCGC_0169 3/13/2014 6,04 5.14 8.0% D Upper Valley CCGC_0169 3/13/2014 5.71 5,16 5.0% D Upper Valley CCGC_0167 3/13/2014 15.44 13.76 5.8% D Upper Valley CCGC_0183 3/13/2014 16.41 13.82 8.6% D/I Pressure CCGC_0131 3/13/2014 19.66 17,48 5.9% D Pressure CCGC_0171 3/13/2014 51.17 45.13 6.3% D Upper Valley CCGC_0172 3/13/2014 28.43 25.80 4.9% D Upper Valley CCGC_0187 3/14/2014 26.77 21.84 10.1% D Forebay CCGC_0174 3/14/2014 15.75 14,46 4.3% D/I Forebay CCGC_0173 3/14/2014 30.44 25.18 9.5% D/I Forebay CCGC_0175 3/14/2014 24,07 18,12 14.1% D Forebay CCGC_0177 3/14/2014 19.18 15.81 9.6% D Forebay CCGC_0176 3/14/2014 20,89 18,32 6.6% D Forebay CCGC_0186 3/14/2014 14.46 11,95 9.5% D Forebay CCGC_0140 3/14/2014 6.52 5.53 8.2% D East Side CCGC_0136 3/14/2014 10.92 9,26 8.2% D Pressure
C-6
Sample ID Date
Sum Cations
(meq /L) Sum Anions
(meq /L) Anion /Cation balance
(% difference) Use Basin
CCGC_0136 3/14/2014 10.87 9.33 7.6% D Pressure
CCGC_0137 3/14/2014 9.07 8.17 5.2% D Pressure
CCGC_0141 3/14/2014 4.90 4.28 6.7% D East Side
CCGC_0138 3/14/2014 33.40 29.89 5.5% I East Side
CCGC_0139 3/14/2014 11.19 10.01 5.6% D/I East Side
CCGC_0191 3/19/2014 12.65 11.70 3.9% D Forebay
CCGC_0193 3/19/2014 26.30 24.25 4.0% D Pressure
CCGC_0197 3/19/2014 4.70 6.28 -14.4% D Forebay
CCGC_0188 3/19/2014 10.63 9.91 3.5% D Forebay
CCGC_0207 3/19/2014 8.79 8.26 3.2% D Forebay
CCGC_0195 3/19/2014 20.71 19.24 3.7% D Forebay
CCGC_0206 3/19/2014 12.50 11.68 3.4% D/I Forebay
CCGC_0194 3/19/2014 18.67 18.51 0.4% D East Side
CCGC_0194 3/19/2014 19.69 18.53 3.0% D East Side
CCGC_0189 3/19/2014 4.70 4.34 4.0% D Forebay
CCGC_0198 3/19/2014 8.49 8.02 2.8% D East Side
CCGC_0196 3/19/2014 5.91 5.74 1.5% D Forebay
CCGC_0190 3/19/2014 4.70 4.32 4.2% D Forebay
CCGC_0201 3/20/2014 36.90 35.05 2.6% D Upper Valley
CCGC_0203 3/20/2014 45.01 42.15 3.3% D Upper Valley
CCGC_0204 3/20/2014 18.86 18.36 1.3% D Upper Valley
CCGC_0200 3/20/2014 26.50 25.60 1.7% D Upper Valley
CCGC_0365 4/29/2014 7.77 7.41 2.3% D East Side
CCGC_0378 5/1/2014 3.88 3.54 4.6% D Pressure
Penny_Irr 7/15/2014 6.49 6.15 2.8% I East Side
Penny_Irr 7/15/2014 6.36 6.12 1.9% I East Side
We1121_Irr 7/15/2014 6.90 6.75 1.1% I East Side
0489_D/I 7/16/2014 2.54 2.44 2.2% D/I Langley
Clausenl_ 7/17/2014 5.90 6.31 -3.4% I Upper Valley
Clausen_D 7/17/2014 8.27 8.78 -3.0% D Upper Valley
Clausen_D 7/17/2014 8.31 8.76 -2.6% D Upper Valley
CCGC_0390 8/6/2014 9.14 9.35 -1.1% D Upper Valley
CCGC_0391 8/6/2014 36.46 37.93 -2.0% D Upper Valley
CCGC_0392 8/6/2014 21.67 22.33 -1.5% D Forebay
CCGC_0393 8/6/2014 14.57 14.71 -0.5% D/I Forebay
CCGC_0396 8/6/2014 37.36 36.65 1.0% D Forebay
CCGC_0395 8/6/2014 52.84 51.89 0.9% D Forebay
CCGC_0394 8/6/2014 44.25 44.33 -0.1% D Forebay
CCGC_0397 8/7/2014 10.60 10.32 1.4% D East Side
CCGC_0399 8/7/2014 9.11 8.43 3.9% D Pressure
CCGC_0398 8/7/2014 12.24 11.65 2.5% D Pressure
CCGC_0400 8/7/2014 12.51 11.80 2.9% D East Side
CCGC_0401 8/7/2014 8.41 7.76 4.0% D East Side
CCGC_0403 8/7/2014 8.95 8.60 2.0% D/I East Side
CCGC_0402 8/7/2014 10.84 10.38 2.2% D East Side
CCGC_0404 8/7/2014 15.07 14.58 1.6% D Pressure
CCGC_0406 8/7/2014 8.54 8.19 2.1% D/I Pressure
CCGC_0405 8/7/2014 8.92 8.42 2.8% D Pressure
CCGC_0431 8/8/2014 12.48 12.19 1.2% D Forebay
CCGC_0432 8/8/2014 27.74 26.76 1.8% D Forebay
CCGC_0433 8/8/2014 25.77 25.63 0.3% D East Side
CCGC_0430 8/8/2014 5.05 4.84 2.1% D Forebay
CCGC_0444 8/14/2014 4.74 4.52 2.4% D/I Pressure
C-7
Sample ID Date Sum Cations
(meq /L) Sum Anions
(meq /L) Anion /Cation balance
(% difference) Use Basin CCGC_0442 8/14/2014 5.45 5.19 2.5% D/I Pressure CCGC_0443 8/14/2014 8.18 7.75 2.7% D Pressure CCGC_0441 8/14/2014 9.14 9.04 0.5% D/I Pressure CCGC_0512 8/26/2014 11.55 10.59 4.3% D Forebay CCGC_0487 8/26/2014 9.33 8.89 2.4% D Forebay CCGC_0178 8/27/2014 8.52 8.14 2.3% D East Side CCGC_0178 8/27/2014 8.29 8.18 0.7% D East Side CCGC_0471 8/27/2014 13.59 13.17 1.6% D East Side CCGC_0484 8/27/2014 31.93 28.55 5.6% D/I Forebay CCGC_0483 8/27/2014 7.77 7.26 3.4% I Forebay CCGC_0493 8/27/2014 36.24 34.08 3.1% D Forebay CCGC_0491 8/27/2014 31,08 29.31 2.9% D Forebay CCGC_0492 8/27/2014 17.36 16.84 1.5% D Forebay CCGC_0513 8/27/2014 15.99 15.00 3.2% 0 Forebay CCGC_0488 8/27/2014 12.60 11.64 4.0% D Forebay CCGC_0489 8/27/2014 26.22 24.89 2.6% D Forebay CCGC_0490 8/27/2014 9.54 9.15 2.1% D Forebay CCGC_0474 8/27/2014 11.82 11.49 1.4% D East Side CCGC_0473 8/27/2014 9.99 9.62 1.9% D East Side CCGC_0511 8/27/2014 33.44 31.40 3.1% D Forebay CCGC_0475 8/28/2014 11.35 11.54 -0.8% D Pressure CCGC_0502 8/28/2014 47.51 44.45 3.3% D Forebay CCGC_0500 8/28/2014 22.38 21,37 2.3% D Forebay CCGC_0508 8/28/2014 6.10 5.67 3.6% D Forebay CCGC_0509 8/28/2014 16.69 15.25 4.5% D Forebay CCGC_0510 8/28/2014 4,90 4.46 4.6% D Upper Valley CCGC_0503 8/28/2014 18.44 17.73 1.9% D Forebay CCGC_0505 8/28/2014 15.56 14,83 2.4% D/I Forebay CCGC_0514 8/28/2014 22.96 21.50 3.3% D Forebay CCGC_0507 8/28/2014 34.98 32.97 3.0% D Forebay CCGC_0056 8/28/2014 19.47 18.73 1.9% D Pressure CCGC_0059 8/28/2014 15.08 14.64 1.5% D Pressure CCGC_0476 8/28/2014 19.04 19,59 -1.4% D East Side CCGC_0477 8/28/2014 13.34 13.71 4.4% D East Side CCGC_0496 8/28/2014 7,93 7.64 1.9% D/I East Side CCGC_0498 8/28/2014 22,54 22.51 0.0% D Forebay
Ratio of Calculated Sum of Dissolved Solids to Specific Conductance
The ratio of the calculated sum of dissolved solids (mg /L) to specific conductance was calculated. The ratio was calculated as follows:
Sum of dissolved solids in mg /L Specific conductance
The sum of dissolved solids divided by the specific conductance should fall within the range 0.55 to 0.81, 55 of the 247 samples (22 percent) do not fall within this range.
C-8
Ratio of the Sum of Reacting Constituents to Specific Conductance
The ratio of the sum of reacting cations (meq /L) to 0.01 times specific conductance, as well as the sum of
reacting anions (meq /L) to 0.01 times specific conductance, should be within the range 0.92 to 1.242. This
ratio was calculated as follows:
Sum of reacting cations (or anions)in meq /L
0.01 x Specific Conductance
Of the 247 samples, 26 (11 percent) do not fall within the range for cations and 15 (6.1 percent) do not fall
within the range for anions.
Laboratory Flags
Two wells have associated laboratory flags that deal with nitrate, summarized in the following table.
WellCOde SampleDate SampleTypeCode LabSamplel6 Replicate LabReplicate QACode
CCGC_0163 3/11/2014 MS1 AB12790+LFM 1 1 BC, LM
AB12790+LFMD 1 2 BC, LM
CCGC_0492 8/27/2014 MS1 AB199234 MS 1 1 BC, LM
AB19923+MSD 1 2 BC, LM
QA Code Description
BC Matrix spike out of control, lab control sample within limits
LM MS and /or MSD above acceptance limits. See Blank Spike(LCS).
An extensive review of the laboratory QA /QC data will be available in the Groundwater Characterization
Report.
Appendix D - CCGC Sampled Well Information and Results
Analytical results for all wells sampled in the Salinas Valley under Characterization Monitoring can be found in the following tables.
Any data excluded from the analysis can be found in Appendix B.
FleidPÓiqtNanle"
CCGC 0001
CCGC 0002
CCGC_0003
CCGC0017
CCGC_0018
CCGC_0019
CCGC_0020
CCGC0021
CCGC_0023
CCGC_0024
CCGC_0026
CCGC_0027
CCGC_0028
CCGC_0029
CCGC 0030
CCGC 0031
CCGC 0032
CCGC_0033
CCGC_0034
CCGC 0035
CCGC_0036
CCGC 0037
CCGC_0038
CCGC_0039
CCGC_0040
CCGC0041
CCGC 004-
CCGC _
CCGC_ _-
CCGC_==-
CCGC_0047
CCGC_0D48
CCGC_='_-5
CCGC CIO
CCGC_0052
CCGC0053
CCGC_0054
CCGC 0055
CCGC_0D56
CCGC_0056
« 0057
___ _0058 CCG __
CCGC ___
_
CCGC0064 LCGC 0065
Tû? Óf_ 9áketp Sc
Of réenxedn ,iened
IntéYval dnterael VellDëplh 5áv4)30áté AriálYtaNáme
24/Oct/2013 Nitrate as NO3
24/Oct/2013 Nitrate as NO3
24/Oct/2013 Nitrate as NO3
22/Oct/2013 Nltra:e e
21/OC21/Oct/2013 Nitra_ as'.CS
5/Oct/2013 Nitra :e as %CE
ITLE Nitrate as NOS _n :
:40 400
100 120
D 140 200
:15 Nitrate as NCE
--- a Nitrate as NUE
NR 21/006/2013 Nitrate as NO3
NR 25/Oct/2013 Nitrate as NO3
NR 21/OC[/2013 N trate as NO3
25 /Oct /2013 =[e as NO3 __- --_.. 2323/Oct/2013 ae as NO3
5 /Oct /2013 .. =as N_5
22/Oct/2013 =.= as N 1
:1 /Oct /2013 Nitrate as N_ .. _..
11/Oct/2013 Nitrate as UE
24/Oct/2013 Nitrate as NCI 21/Oct/2013 Nitrate as NOS -NN .. 7...77 20013 Nitra s'CI .NIN3.. __. _? Cc: 2013 Nitra :B
2013 Nitra as
- C:: 2013 Nitra es\CE
24 /Oct /2013 Nitrate as NO3
24/Oct/2013 Nitrate as NO3 23 ACON 24/Oct/2013 as = :e as NO3 =_
24/Oct/2013 =te as NO3 NAI2_ 24/Oct/2013 1. :-ste as NO3
24/Oct/2013 '. trate as NT_ trate _ 22/OC[/200 13 Nitrate as N'= 25/Oct/2013 T Nitrate as N.-7E
97
296
- -E
e;pló
21
AÇo ai' ^ cutcodai GW Bénin - -
SALINAS VALLEY 180 /400 FOOT AQUI __ SAUNAS S VALLEY FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY EAST SIDE AQUIFER
_ _NINA_. .__NINA
_ SALINAS VALLEY -EAST SIDE AQUIFER
VALLEY ___..._... _...-
--= I SALINAS - FOREBAY AQUIFER
'.one _INAS VALLEY -OE O_IFER
'.one SL_INAS .
V ALL. EY _
-.IFER
' -one - INAS VALLEY E1E-E. E- C_IFER
-. -e SA -I.= 180 /400 FOOT AQUI='_=
----= SA_ -= .? FOREBAY AQUIFER
.--= SA_ -_= I. =__E`- 180 /400 FOOT AQUI=_=
None VALLEY UPPER VALLEY AQUIFER _None LINA-_
_ None _= LINAS VALLEY - FOREBAY AQUIFER Non "' -
-
- None 5:LINAS VALLEY - FOREBAY AQUIFER
None I =LINAS VALLEY - UPPER VALLEYAQUI=
None SALINAS VALLEY EAST SIDE AQUIFER
= None SAUNAS VALLEY - EAST SIDE AQUIFER _.._.__
S=LINAS VALLEY - FOREBAV AQ_ =E=
c-a 5-n UNAS VALLEY- 180 /400 FÓ0
-"LINAS VALLEY - EAST SIDE Aq =_?
SOLI NAS VALLEY - EAST SIDE AQ_ F_= 00__._. SALINAS VALLEY - 186 0/400 FOOT AQUI=_=
_' LINAS VALLEY FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS AQUI_
S VALLEY - FOREBAY AQUIFER
ZFLINAS VALLEY -FOREBAYAQUIFER
S =LINAS VALLEY - FOREBAY AQUIFER
S=LINAS VALLEY - FOREBAY AQUIFER
22/Oct/2013 Nitrate as NO3 ANeA__
22/Oct/2013 Nitrate as NO3 _ate 21/Oct/2013 Nitrate as NO3
22/Oct/7013 Nitrate as NO3
22/Oct/2013 Nitrate as NO3 C_
22/Oct/2013 Nitrate as NO3
25/ /OCt/2013 Nitrate as NO3
24/Oct/2013 Nitrate as NOS
24/Oct/2013 Nitrate as NOS
24 Oct /2013 Nitrate as NOI /2013 Nitrate as NO'_
/2013 Nitrate as NO3 .ate - Cc: /2013 Nitrate as NO3
-_ : ::/2013 Nitrate as NO3
23/Oct/2013 Nitrate as NO3
23/Oct/2013 NO3 13 Nitrate as N
23/Oct/2013 Nitrate as NOS
24/Oct/2013 Nitrate as N-5 24/Oct/2013 Nitrate as NOS
23/0Cí/22013 Nitrate as NOS .NI 23/OCV2. 13 Nitrate as .I 21/Oct/2013 Nitrate as NO'_ -_- 23/Oct/2013 Nitrate as NO3
400 23/0ct/2013 Nitrate as NO3
400 28/Aug/2014 Nitrate as NO3
441 23/Oct/2013 Nitrate as NO3 ___. .. .. ___. 180 25/Oct/2013 Nitrate as NO3
--' 23/Oct/2013 =e=_'.03
28/A4/2014 -aa'-03
23/0c: ET LE 1 Nitr= -e= 23/0c:-:::: I Nitrsse _.'.C3 23/0c: :TIE Nnr -BE'C'S 22/002/2013 Nitrate as N_: 22/Oct/2013 Nitrate as NOI
22/0e: 2:1E Nitrate as NOS
25/00: CS Nitrate as NOE rate -_.
22 /0Cr L'.11E Nitrate as N]3
_ALLEY - FOREBAY __ AQUIFER
-_ -ALLEY - 180/400 FOOTAQUI'E2
?.ALLEY 180 /400 FOOT AQUI='_=
S =LINAS VALLEY - EAST SIDE AQUIFER
INAS VALLEY EAST SIDE AQUIFER
_4_INAS VALLEY - 180/400 FOOT AQUI='_=
nAL INA S VALLEY - 1180 00/4_40.__0 FO OT AQUIFER
SALINAS VALLEY- 160 /400 FOOT AQ UIFER -_.
S =LINAS VALLEY - 180 /400 FOOT AQUIFER I
AL _ 180/ ANNA. c'LINAS VALLEY 180 /400 FOOT AQUIFER j
ScLINAS VALLEY - FOREBAY AQUIFER ANNA_ . EY
-=LINAS VALLEY - FOREBAY AQUIFER __NINA FOREBAY NINA_ VALLEY FOREBAY AQUIFER ANNA
LINAS VALLEY F REeAV AQUIFER
NAS VALLEY AY AQUIFER
-
L NAS VALLEY : c:O FOOT AQUIFER
'---_ S =LINAS VALLEY- - =_0 :0 FOOT AQUIFER
None SALINAS VALLEY 180 /400 FOOT AQUIFER __. None SALINAS VALLEY - 180/400 FOOT AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
.= a SALINAS VALLEY FOREBAY AQUIFER.
-e SALINAS VALLEY -FOREBAYAQUIFER
-= SALINAS VALLEY FOREBAYAQUIFER SALI_ IFERA_
SAUNAS VALLEY -FOREBAY AQUIFER
SALINAS VALLEY - 180/400 FOOT AQUI =EP
SAUNAS VALLEY - EAST 510E AQUIFER
None SALINAS VALLEY- 180 /40D FOOT AQUIFER
None SALINAS VALLEY -01 : =00 FOOT AQUI'EP
None S =LINAS VALLEY- __ =00 FOOTAQUI=E4 N
_V
None -=UNAS VALLEY -'_'VALLEY A4UI ='=- _.
--_ - UNAS VALLEY _ "00 FOOT AQUIFER
SALINAS VALLEY - __ =00 FOOT AQUIFER j
S ALINAS VALLEY s : =00 FOOT AQUIFER
-- .1:1 .ALLEY AV AQUIFER . -e _ -ALLEY E= VALLEY AQUI=E=
' t-5 --ALLEY _ r.sAY AQUIFER
SALINAS VALLEY FOREBAYAQUIFER
- -e SALINAS VALLEY - UPPER VALLEYAQUI=E=
'---- SALINAS VALLEY UPPER VALU T. -- SALINAS VALLEY FOREBAYAQ=
:-a SALINAS VALLEY -180 /400 F07-11._ _=
FleldPaintName J Use Top Of
Screened Bottom L Screened WellPepth SampleDate AnalyteName Result
ResQual Code
oACade 6W Basin Interval Interval
CCGC 0069 D 400 440 595 21/Oct/2013 Nitrate as NO3 0.9 None SALINAS VALLEY - 130/400 FOOT AQUIFER
CCGÇ 0070 NR 21/Oct/2013 Nitrate as NO3 9 None SALINAS VALLEY -180/400 FOOT AQUIFER 418 424
CCGC_0071 D V 410
470 446
487
512 25/Ott/2013 Nitrate as NOI 2 None SAUNAS VALLEY -150/400 FOOT AQUIFER
CCGC_0072 D I '. 400 23/Oct/2013 i Nitrate as NO3 7 None SALINAS VALLEY FOREBAY AQUIFER CCGC_0073 D I 400 25/Oct/2013 Nitrate as NO3 21 None SALINAS VALLEY - FOREBAY AQUIFER _ ._. IFE. CCGC_0074 D1 250 23/Oct /2013 Nitrate as NO3 156 None SAUNAS VALLEY FOREBAY AQUIFER CCGC_0075 DI 200 23/0cV2013 Nitrate as NO3 92 None SALINAS VALLEY - FOREBAY AQUIFER CCGC_0107 NR 10 /Mar /2014 Nitrate as NO3 486 None SALINAS VALLEY - EAST SIbE AQUIFER CCGC_0108 271 309 326 10 /Mer /2014 Nitrate as NO3 4 None SALINAS VALLEY - CORRAL DE TIERRA AREA [CGC 0109 360 400 SOD 10 /Mar /2014 Nitrate as NO3 1 None SALINAS VALLEY -180 /400 FOOT AQUIFER ALLE CCGC_0110 NR 10 /Mar /2014 Nitrate as NO3 <1 ND None ' SALINAS VALLEY -180 /4400í00T AQUIFER CCGÇ 0111 NR 10 /Mar /2014 Nitrate as 1103 3 None SAUNAS VALLEY 180 /400 FOOT AQUIFER CCGÇ 0112 NR 10 /Mar /2014 Nitrate as NO3 11 None SALINAS VALLEY 180 /400 FOOT AQUIFER CCGC_0113 I NR 11/Mar/2014 Nitrate as NO3 60 None SALINAS VALLEY -180/400 FOOT AQUIFER CCGC_0114 317 11 /Mar /2014 Nitrate as NO3 <1 ND None SALINAS VALLEY -180 /400 FOOT AQUIFER CCGÇ 0115 D NR 11/Mar/2014 Nitrate as NO3 172 None SALINAS VALLEY - EAST SIDE
_._ CCGC_0116 D NR 11 /Mar /2014 Nitrate as NO3 174 None SALINAS VALLEY - EAST SIDE AQUIFER CCGC_0117 D NR 11 /Mar /2014 Nitrate as NO3 41 ND None SALINAS VALLEY -180/400 FOOT AQUIFER CCGÇ0118 NR 11 /Mar /2014 Nitrate as NO3 <1 ND None SALINAS VALLEY -180/400 FOOT AQUIFER CCGC_0120 D NR 11 /Mer /2014 Nitrate as NO3 I 13 Nane SALINAS VALLEY -180 /400 FOOT AQUIFER CCGC0121 NR 12/Mar/2014 Nitrate as NO3 I 209 None SALINAS VALLEY - EAST SIDE AQUIFER CCGC_0122 NR 12/Mar/2014 Nitrate as 1403 106 None SALINAS VALLEY -180 /400 FOOT AQUIFER CCGC_0123 NR 12 /Mar /2014 Nitrata as NO3 249 None SALINAS VALLEY - 180/400 FOOT AQUIFER CCGÇ0124 119 135 152 12 /Mar /2014 Nitrate as NO3 114 None SALINAS VALLEY - EAST SIDE AQUIFER CCGÇ0125 NR 12/Mar/2014 Nitrate as NO3 177 None SALINAS VALLEY EAST SIDE AQUIFER CCGÇ0126 D 1010 12/Mar/2014 Nitrate as NO3 ! 1 Nane SALINAS VALLEY - 180 /400 FOOTAQUIFER CCGC_0127 D 780 12 /Mar /2014 Nitrate as NO3 2 None SALINAS VALLEY - 180/400 FOOT AQUIFER CCGÇ0128 D 780 12 /Mar /2014 Nitrate as NO3 2 None SALINAS VALLEY °180 /400 FOOT AQUIFER CCGC_0129 S5 170 175 12 /Mar /2014 Nitrate as NO3 <1 ND None SALINAS VALLEY - IANGLEY AREA CCGC_0131 NR 13/Mar/2014 Nitrate as NO3 79 None SALINAS VALLEY -180 /400 FOOT AQUIFER CCGC_0132 __.. -__ 200 13/Mar/2014 Nitrata as NO3 <1 ND None SALINAS VALLEY SEASIDE AREA CCG C_0133 437 452 460 13/Mar/2014 . Nitrata as NOS 18 None SALINAS VALLEY - 180 /400 FOOT AQUIFER CCGÇ0134 NR 13/Mar/2014 Nitrata as NO3 2 None SAUNAS VALLEY - 180/400 FOOT AQUIFER CCGÇ 0135 NR 13/Mar/2014 Nitrate as NO3 19 None SALINAS VALLEY -180/400 FOOT AQUIFER CCGC_0138 480 580 589 14 /Mer /2014 Nitrate as NOS 10 ' None SALINAS VALLEY 180/400 FOOT AQUIFER CCGCs0137 230 14/Mar/2014 Nitrate as NO3 6 None SAUNAS VALLEY - 180/400 FOOT AQUIFER CCGC_0138 640 14/Mar/2014 Nitrate as NO3 690 None SALINAS VALLEY - EAST SIDE AQUIFER
260 312 CCGC_0139 DA
360 450 500 14/Mar/2014 Nitrate as NO3 191 None SALINAS VALLEY - EAST SIDE AQUIFER
CCGC_0140 580 660 .. 900 14/Mer/2014 Nitrate as NO3 4 None SALINAS VALLEY - EAST SIDE AQUIFER CCGC_0141 660 14 /Mar /2014 Nitrate as NOI 6 None
_.. __. SAUNAS VALLEY - EAST SIDE AQUIFER
CCGC_0142 NR 10 /Mer /2014 Nitrate as NO3 30 None SALINAS VALLEY - FOREBAY AQUIFER CCGC_0143 NR 10 /Mar /2014 Nitrate as NO3 92 None SALINAS VALLEY - FOREBAY AQUIFER CCGC_0144 410 10 /Mar /2014 I Nitrate as NOI 2 None SALINAS VALLEY FOREBAY AQUIFER CCGC_0145 NR 10 /Mar /2014 Nitrate as NOS 19 None SALINAS VALLEY- 180 /4D0 FOOTAQUIFER CCGC_0146 NR 10 /Mar /2014 Nitrate as NO3 22 None SALINAS VALLEY - 180/400 FOOTAQUIFER
. CCGC_0150 NR 11 /Mar /2014 Nitrate as NOI : 36 None SALINAS VALLEY - FOREBAY AQUIFER CCGC_0151 NR 12/Mar/2014 Nitrate as NO3 19 None SALINAS VALLEY - FOREBAY AQUIFER CCGC 0152 NR 11 /Mar /2014 Ntrate as NO3 20 None SAUNAS VALLEY - FOR EBAY AQUIFER CCGÇ0153 NR 11 /Mar /2014 Nitrate as NO3 239 None SALINAS VALLEY- UPPER VALLEY AQUIFER __. CCGC_0155 NR 11/Mar/2014 Nitrate as NO3 76 None SALINAS LLEVAFOREBAY AQUIFER _.. __. CCGC_0156 NR 11 /Mar /2014 Nitrate as NO3 182 None SALINAS VALLEY °FOREB EBAY AQUIFER CCGC_01S7 NR 11 /Mer /2014 Nitrate as NO3 106 None SALINAS VALLEY - FOREBAY AQUIFER CCGÇ 0158 NR 11 /Mar /2014 Nitrate as NO3 62 None SALINAS VALLEY ° FOREBAY AQUIFER CCGÇ 0159 NR 12/Mar/2014 Nitrate es NO3 9 Nane SALINAS VALLEY - 180/400 FOOTAQUIFER CCGC_0160 NR 12 /Met /2014 Nitrate as NO3 205 None SALINAS VALLEY - FOREBAY AQUIFER CCGÇ 0161
'. NR 12/Mar/2014 Nitrate as NO3 112 None SAUNAS VALLEY - FOREBAY AQUIFER CCGC 0162 NR 11 /Mar /2014 Nitrate as NO3 46 None SALINAS VALLEY - FOREBAY AQUIFER CCGC 0163 NR 11 /Mar /2014 Nitrata as NOS 482 None SALINAS VALLEY UPPER VALLEY AQUIFER CCGÇ 0164 220 400 400 11 /Mar /2014 Nitrate as NOS 221 None SALINAS VALLEY - FOREBAY AQUIFER CCGÇ D165 NR 12/Mar/2014 Nitrate as NO3 97 None SALINAS VALLEY - FOREBAY AQUIFER CCGÇ 0166 NR 13 /Mer /2014 Nitrate as NO3 28 None SALINAS VALLEY - UPPER VALLEY AQUIFER CCGC0167 NR 13/Mar/2014 Nitrata as NO3 178 None SALINAS VALLEY - UPPER VALLEY AQUIFER CCGC_0168 NR 13 /Mar /2014 . Nitrate ea NOI 111 None SALINAS VALLEY - UPPER VALLEY AQUIFER 000Ç 0169 NR 13 /Mer /2014 Nitrate as NO3 20 None SALINAS VALLEY - UPPER VALLEY AQUIFER ccGC_ó170 NR 13 /Mar /2014 Nitrate as NO3 230 None SALINAS VALLEY- UPPER VALLEY AQUIFER CCGC_0171 NR 13/Mar/2014 Nitrate as NO3 146 None SALINAS VALLEY - UPPER VALLEY AQUIFER CCGÇ 0172 NR 13 /Mar /2014 Nitrate as N63 <1 ND None SALINAS VALLEY - UPPER VALLEY AQUIFER CCGÇ 0173 NR 14 /Mar /2014 Nitrate as NO3 166 None SALINAS VALLEY - FOREBAY AQUIFER CCGC_0174 NR 14 /Mar /2014 Nitrate as NOI 78 None SALINAS VALLEY - FOREBAY AQUIFER CCGÇ 0175 NR 14 /Mar /2014 Nitrate as NO3 168 None SALINAS VALLEY - FOREBAY AQUIFER
4
FlêláVointNarile
CCGC0176
I CCGC_0177
CCGC_0178
CCGC_0178
_CGC 0179
___0180 0181
CCG_186 CCGC0187
C:3:10188 C
- 0189
C=_=_0190
C__- 0191
_- 0193
CCGC= _
CCGC =_E7
CCGC_0198
CCGC_0200
CCGC_0201
CCGC_0203_
CCGC 0204
CCGC_0206
CCGC_0_207
- CCGC_0365
CCGC -- 0378 ..i..-_..__
CCGCz0386_
CCGC_0387
CCGC_039D
CCGC0391 CCGC - 0392
CCGC_0393
CCGC_0394
CCGC 3EI
..CCGC 32= CCGC 3= CCGC_CEES
CCGC_0399
CCGC_0400
CCGC_040_1
CCGC_0402
CCGC 0403 1 CCGC 0404
CCGC 0403 li
CCGC_0406
COGC_0430 ._... CCGC_0431_
_= 0432
-Z2 0433 .__ 0:1:_0441
D
D
O
Topol.'80{túinPf Sereénétl Sagene8 WelÓepth
etterral 'nteiyel
CCGC_0442 D/I
CCGC =A-E
CCGC__--
CCGC_== CCGC_0473
CCGC_0474
CCGC_0475
CCGC_0476
CCGC_0477
CCGC_0483
CCGC_0484
CCGC 0487
CCGC_0488
320 360
530
AnalyteNátné
:4 /Mar'2C_! :-a :e as NZE
_4 /Mar _= . :-ate as NZ.-3
:2/Mar/2014 Nitrate as NCS
17/Aug/2014 Nitrate as N'5 -I _.._ 2 /Mar /2014 Nitrate as
s N_
2 /Mar /2014 Nitrate as NO3 -
12 /Mar /2014 Nitrate as NO3 E
E3/Mar/2014 Nitrate as NO3 __ __.
3 /Mar /2014 Nitrate as N? 3 /Mar /2014 Nitrate as N.E 3 /Mar /2014 Nitrate as NCE
4/Mar/2014 Nitrate as NC'_
NOS Nitrtrate e
N- as _ ?
19 /Mar /2014 Nitraté as N__ - -- _.._ 19 /Mar /2014 Nitrate asN 28
_...___. _-. __._.
1 9 /Mar /2014 Nitrate as N_3 10 ___.. :9/Mar/2014 Nitrate as N.E 188
9 /Mar /2014 Nitrate as NO3 202
3/Mar /2014 Nitrate as NO3 454
:9/Mar/2014 =_ ZE {- 9/Mar/2014 = -- 9 /Maar /201_4 - _
9/Mar /2014 rare as
0 /Mar /2014 Nitrate as N.T.S.
0 /Mar /2014 Nitrate as N =E
20 /Mar /2014 Nitrate as NC6
20 /Mar /2014 Nitrate as N =6
3 /Mar /2014 Nitrate as NOI
/Mar /2014 Nitrate as N_9 _.._ 29/Apr/2014 Nitrate as NO3 I
01/May/2014 Nitrate as NO3
06 /Aug /2014 Nitrate as' -J'_
O6 /Aug /2014 Nitrate as N.73
_6 /Aug /2014 Nitrate as N]5 :6 /Aug /2014 Nitrate as N =: C6 /Aug /2014 Nitrate as N =6
=6 /Aug /2014 Nitrate as NOI
:6 /Aug /2014 Nitrate as NO3 362
Q{sCOdé`GY4`e$s1q.,^ "` ;°` .- . .
-:-a SA_ -AS-ALLEY -FOREBAYAQUIFER
SA_': 5 -ALLEY FOREBAYAQUIFER
'.one EL_ --AE .ALLEY -EAST SIDE AQUIFER
tone ALLEY - EAST SIDE AQUIFER
' -one -E -ALLEY FOREBAY AQUIFER
None SALINAS VALLEY UPPER VALLEYAQUI =E=
None SALINAS VALLEY UPPER VALLEY AQUI='_=
Ncne SALINAS VALLEY - 180 /400 FOOTAQUI =E=
.re SALINAS V: - 180 /400 FOOT AQUIFER
SALINAS V= -E- 180 /400 FOOT AQUIFER . -0 -" AQUIFER '--= SAUNAS VL___ - 180 /400 FOOT AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
' -one SALINAS VALLEY FOREBAYAQUIFER
'.one SALINAS VALLEY - FOREBAY AQUIFER
'.one SALINAS VALLEY AQUIFER AQUIFER
'.one SALINAS VALLEY FOREBAY AQUIFER
'.one SALINAS VALLEY =-Y AQUIFER
'one SAUNAS VALLEY no FOOTAQUP'_'. '
SALINAS VALLEY- E DE AQUIFER - -_ _.._- r SALINAS VALLEY AQUIFER
--- SALINAS VALLEY FOREBAY AQUIFER
.re SALINAS VALLEY FOREBAYAQUIFER
'.one SALINAS VALLEY EAST SIDE AQUIFER
'.one SALINAS VALLEY UPPER VALLEY AQUIFER
'.one SALINAS VALLEY UPPER VALLEY AQUIFER
'rana SniNAS VALLEY UPPER VALLEY AQUIFER
'.one SALINAS VALLEY - UPPER VALLEY AQUIFER
:one SALINAS VALLEY FOREBAY AQUIFER
'.one SALINAS VALLEY -FOREBAYAQUIFER
'.one EALINAS VALLEY EAST SIDE AQUIFER
SALINAS VALLEY - 180/400 FOOT AQUI =E=
SALINAS VALLEY - PASO ROBLES AREA __NASA_ PASO '.one SALINAS VALLEY PASO ROBLES AREA
V_ UPPER SALINAS VALLEY VALLEN AQUI=_
SALINAS SALINAS VALLEY UPPER VALLEY AQUI=_ SALINAS VALLEY - FOREBAY AQUIFER _..__....__ "
FOREBAY SALINAS VALLEY FOREBAY AQUIFFER
-.one SALINAS VALLEY- FOREBAY AQUIFER
_6 /Aug /2014 Nitrate as N :: :6/Aug/2014 Nitrate as NCE
:7 /Aug /2014 Nitrate as N =E
7/Aug /2014 Nitrate asN_- _7 /Aug /2014 Nitrate as N^ 07/Aug/2014 Nitrate as N-'_ 07/Aug/2014 Nitrate as N =6
07/Aug/2014 Nitrate as
Nitrate_ as N=`_
07 /Aug /2014 Nitrate as N :E 07 /Aug /2014 Nitrate as NIE 07 /Aug /2014 Nitrate as NCE
08/Aug/2014 Nitrate as NC6
08 /Aug /2014 Nitrate as N =E
08 /Aug /2014 Nitrate as N =E
:8 /Aug /2014 Nitrate as NO:
14 /Aug /2014 Nitrate as N =E
487
218
14/AUg/2014 Nitrate as N5 1
370 14/Aug/2014 Nitrate as Not
14 /Aug /2014 Nitrate as N=E <1
A -.3/2014 Nitrate as N-'_ -__/2014 Nitrate as NO3
_- A _/2014 Nitrate as NOS
-S/2014 Nitrate as NOE
o Á_g/2014 Nitrate as N :E 614
400 =E A-_/2014 Nitrate as N:; 25
'.one SALINAS VALLEY - AQUIFER
None SALINAS AS VALLEY- FOREBAV AQUIFER
None SALINAS VALLEY EASTSIDEAQUIFER
re SALINAS VALLEY 180 /400 FOOT AQUI A=
SALINAS VALLEY 180 /400 FOOT AQUI E_
c SALINAS VALLEY - EAST SIDE AQUIFER __._.D_. '--= SALINAS VALLEY EAST SIDE AQUIFER -
-= SAUNAS VALLEY - EAST SIDE AQUIFER
SALINAS VALLEY - EAST SIDE AQUIFER
'one SALINAS VALLEY 180 /400 FOOT AQUI _. None SALINAS VALLEY 180 /400 FOOT AQUIFER
None SALINAS VALLEY - 180 /400 FOOT AQUIFER '
_.. -.. SALINAS VALLEY FOREBAY AQUIFER
LINAS VALLEY AQUIFER
VALLEY ._..
',_ n"LINAS VALLEY FOREBAV AQUIFER INS ---- SALINA3 VALLEY EAST E
SALINAS VALLEY 180 /4_: :: AQUI =E=
None
None
None
None
None
None
None
None
SALINAS VALLEY - 180 /400 FOOT AQUIFER
SALINAS VALLEY 180 /400 FOOT AQUIFER
SALINAS VALLEY - 180/400 FOOT AQUI =Er
LINAS VALLEY - EAST SIDE AQUIFE=
< LINAS VALLEY EAST SIDE AQ_ _E_
SALINAS VALLEY - EAST SIDE AQ_ _'_'
LINAS VALLEY - 180/400 F00 ,_ __ SALINAS VALLEY - EAST SIDE AQUIFER
None 3ALINAS VALLEY EAST SIDE AQUIFER
NR 27 /Aug /2014 Nitrate as N:3 16 None 5 LINAS VALLEY - FOREBAYAQUIFER
'.= 27/Aug /2014 Nitrate as ACE Aé None SALINAS . -_=* FOREBAY AQUIFER
26 /Aug /2014 Nitrate as N _ EE = None SALINAS -.- FOREBAYAQUIFER
27 /Aug /2014 Nitrate as N - _E None 3ALINAS .A FOREBAYAQUIFER
Bottom (n Screened Interval
210
QACode
None
None
None
None
None
None
None
None
None
None
None
None
None
None
None
None
None
None
None
FIeidPoIntNeme I Use
CCGC_0489 D
CCGC0490 D
CCGC_0491 D
CCGC 0492 . D
CCGC_0493 D _... _-. . _. CCGC 0496 ! Dfl '.
CCGC 0498 D
CCGC0500 D
CCGC0502 ' D
CCGC 0503 D
CC6C_0505 ' D/I
CCGC_0507 0 CCGC 0508 D
CCGC_0509 D
CCGC0510 I _
D
CCGC0511 D
CCGC0512 D
CCGC 0513 D
CCGC 0514 0
Top Of Screened Interval
190
WellOepth
NR
NR
147
NR
NR
NR
NR
NR
NR
NR
NR
NR
NR
NR
NR
NR
210
NR _.. NR
I Samplepate
27/Aug/2014 27/Aug/2014 ¡
27/Aug/2014 27/Aug/2014 27/AUg/2014
28(A0g/2014
28/Aug/2014 28/Aug/2014
28/Aug/2014 28/Aug/2014
28/Aug/2014 28/Aug/2014 28/AUg/2014
28/Aug/2014 28/Aug/2014 27/Aug/2014
26/Aug/2014 27/Aug/2014
28/Aug/2014
ResQual AnalyteName I Result
Cgde
Nitrate as NO3 239
Nitrate at Nos - 116
- NitrateasNO3 398 ._. ...
Nitrate as NO3 95
Nitrate as Nos 511
Nitrate as NOS 23
Nitrate as NOs 51
Nitrate as NOS 256
Nitrate as NO3 84 ._.__. . ... Nitrate as N°3 286
Nitrate as NO3 186
Nitrate asNO3 , 346
Nitrate as Nos 12
Nitrate as NO3 144
Nitrate es NO3 2
Nitrata as Nos 198
; Nitrate as NO3 93
Nitrate as 47 ._.. Nitrate as NO3 349
GR/Basin
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - EAST SIDE AQUIFER SALINAS VALLEY FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY FOREBAY AQUIFER SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY UPPER VALLEY AQUIFER SALINAS VALLEY - FOREBAY AQUIFER SALINAS VALLEY - FOREBAY AQUIFER SALINAS VALLEY - FOREBAY AQUIFER
SALINAS VALLEY - FOREBAY AQUIFER
pleQ
i C
CG
C_0
001
24/O
ct/2
013'
A
lkal
inity
as
CaC
O3
239
I N
one
CC
GC
_000
1 24
/Oct
/201
3 B
icar
bona
te
292
Non
e
CCGC_0001
24/Oct/2013
Calcium
134
Non
e _
CC
GC
_000
1 _
__
24/O
ct/2
013
Chl
orid
e 57
N
one
CC
GC
00
01
24/O
ct/2
013
Har
dnes
s as
CaC
O3
475
Non
e
CC
GC
_000
1 24
/Oct
/201
3 M
agne
sium
34
N
one
CC
GC
_000
1 24
/Oct
/201
3 5
Non
e N
itrat
e +
Nitr
ite a
s N
0[6[
_000
1 C
G
24/0
[!/20
13
Nitr
ate
2.2.
22_.
_...
Nitr
ate
as N
OS
-N
2227
4.
7 N
one
CC
GC
_000
1 24
/Oct
/201
3 N
itrite
as
NO
2 -N
0.
3 N
one_
__
CC
GC
_000
1 24
/0ct
/201
3 P
otas
sium
3.
8 N
one
0[6[
_000
1 24
/Oct
/201
3 S
odiu
m
55
=
Non
e
0[6[
_000
1 24
/0ct
/201
3 S
peci
ficco
nduc
tivity
10
15
=
i N
one
0[6[
_000
1 24
/Oct
/201
3 S
ulfa
te
193
=
Non
e
CC
GC
0001
24
/Oct
/201
3 T
otal
Dis
solv
ed S
olid
s 70
0 =
N
one
0[6[
_000
2 24
/OC
t/201
3 A
lkal
inity
as
CaC
O3
237
=
Non
e
CC
GC
_000
2 24
/005
/201
3 B
icar
bona
te - -- _
28
9 =
N
one
CC
GC
00
02
O_.
2013
24
/0[5
/201
3 C
alci
um
Cal
cium
17
9 N
one
CC
GC
_000
2 24
/Oó/
2013
C
hlor
ide
147
=
Non
e
CCGC 0002
24/Oct/2013
. Hardness as CaCO3
649
=
None
0[6[
_000
2 24
/0[[/
2013
M
agne
sium
49
-
Non
e I
CC
GC
00
02
._.
24/O
ó/20
13
Nitr
ate
+ N
itrit
as
N
22.1
_
' N
one
CC
GC
_000
2 24
/0ct
/201
3 N
itrat
e as
N
O3
-N
21.8
=
I
Non
e
CC
GC
_000
2 24
/Oct
/201
3 N
itrite
as
NO
2 -N
0.
3 =
N
one
0[6[
_000
2 24
/Oct
/201
3 P
otas
sium
5.
8 =
,
Non
e
0000
_000
2 24/Oct/2013
Sod
ium
79
=
None
CC
GC
_000
2 24
/Oct
/201
3 ,`
Spe
cific
cond
uctiv
ity
1443
_
Non
e ,
CC
GC
_000
2 24
/Oct
/201
3 S
ulfa
te
219
Non
e 2222
CC
GC
_000
2
_ 13
24/Oó/2013
__.._
T
otal
Dis
solv
ed S
olid
s 93
7 None
;
CC
GC
00
03
24/O
ct/2
013
Alk
alin
ity
ty a
s as C
aCO
3 i
266
Non
e
CC
GC
_000
3 24
/Oct
/201
3 B
icar
bona
te
325
Non
e _
CC
GC
_000
3 24
/Oct
/201
3 C
alci
um
r 27
7 None
CC
GC
_000
3 24
/00t
/201
3 C
hlor
ide
104
None
CC
GC
_000
3 24
/Oct
/201
3 H
ardn
ess
as C
aCO
3 10
38
Non
e
0[6[
_000
3 _.
_
24/O
ct/2
013
Mag
nesi
um
84
Non
e
CC
GC
_000
3 24
/Oct
/201
3 N
itrat
e +
N
itrite
as
N
'
57.1
N
one
0[6[
_000
3 _0
00
- 24
/Oct
/201
3 N
itrat
e as
NO
3 -N
66
.8
Non
e
CC
GC
_000
3 24
/0ct
/201
3 N
itrite
as
NO
2 -N
0.
3 =
N
one
CC
GC
_000
3 24
/Oct
/201
3 P
otas
sium
6.
6 None
CC
GC
00
03
24/O
ct/2
013
Sod
ium
97
=
Non
e
CC
GC
_000
3 24
/Oct
/201
3 S
peci
ficco
nduc
tivity
20
44
-
!
Non
e
[CG
C
0003
24
/00!
/201
3 S
ulfa
te
457
_ _'
None
CC
GC
_000
3 24
/Oct
/201
3 I
Tot
al D
isso
lved
Sol
ids
1523
_
Non
e Ì
CC
GC
_000
4 22
/Oó/
2013
A
lkal
inity
as
CaC
O3
249
_ None
CC
GC
22
/Oct
/201
3 ;
Bic
arbo
nate
30
4 _
Non
e .0
004
0[6[_0004
22/O
ct/2
013
Cal
cium
54
=
None
CC
GC
_000
4 22
/Oct
/201
3 C
hlor
ide
54
_ N
one
CC
GC
_000
4 22
/Oct
/201
3 H
ardn
ess
as C
aCO
3 20
9 _
Non
e
CC
GC
_000
4 22
/Oct
/201
3 M
agne
sium
!
18
=
Non
e
04
CC
GC
_000
4 22
/Oct
/201
3 22
10
Nitr
ate
+ N
itrite
N
te
a
2.4
2022
_._
- !
Non
e -_
- _ -2
222
CC
GC
_000
4 22
/0C
í/201
3 N
itrat
e as
NO
3 -N
2
a N
one
CC
GC
_000
4 22
/Oct
/201
3 I
Nitr
ite a
s N
O2
-N
0.4
_ N
one
CC
GC
00
04
22/O
ct/2
013
Pot
assi
um
2.6
T
a - N
one
CC
GC
00
04
2 22
/0[!/
2013
- -
._
_ 02
00.
Sod
ium
S
odiu
m
70
- _
None
Spe
cific
Con
duct
ivity
65
8 _.
20
22
=
! N
one
0[6[
_000
4 22
/Oct
/201
3
CC
GÇ
0004
22
/Oct
/201
3 S
ulfa
te
9 _
Non
e
CC
GÇ
0004
22
/0cs
/201
3 T
otal
Dis
solv
ed S
olid
s 40
0 I
_ ¡
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e ,
CC
GC
00
05
21)0
0! /2
013
Alk
alin
ity a
s C
aCD
3 20
9 N
one
Ptii
_ie"
F éiz
si;
CC
GC
_000
5 21
/Oct
/201
3 B
icar
bona
te
255
=
Non
e C
CG
C 00
05
21/0
[[/20
13
Cal
cium
10
5 =
N
one
__
_ 2.
222_
._
CC
GC
000
5 21
/Oct
/201
3 C
hlor
ide
84
=
Non
e
CC
GC
00
05
21/O
ct/2
013
Har
dnes
s as
CaC
O3
419
=
Non
e
CC
GC
_000
5 21
/OC
t/201
3 M
agne
sium
38
=
N
one
CC
GC
00
05
21/0
[!/20
13
Nitr
ate
as
7.6
=
Non
e
CCGÇ 0005
21/O
ct/2
013
Nitr
ate
as N
O3-
N
73
=
Non
e
CC
GC
000
5 21
/Oct
/201
3 N
itrite
as
NO
2 -N
0.
3 a
Non
e
CCGÇ 0005
21/0[[/2013
Potassium
4
e None
CC
GÇ
0005
21
/0[!/
2013
S
odiu
m
91,
=
Non
e
CC
GC
00
05
21/O
ct/2
013
Spe
cific
Con
duct
ivity
11
62
=
Non
e
CC
GÇ
0005
21
/OC
t/201
3 S
ulfa
te
246
a N
one
CC
GC
00
05
21/O
ó/20
13
Tot
al D
isso
lved
Sol
ids
820
=
Non
e
CC
GC
00
06
25 /O
ct /2
013
Alk
alin
ity a
s C
aCO
3 25
5 =
N
one
CC
GC
O
OO
fi 2S
/Oct
/201
3 B
icar
bona
te
311
=
None
1_, 0[
6[_0
006
25/0
[!/20
13
Cal
m
168
=
N
e
Cal
.2
..2.2
2....
_.
._
..__.
. .2
222.
0[6[_0006
25 /O
ct /2
013
Chl
orid
e 80
=
None
L C
CG
C
0006
25
/Oct
/201
3 H
ardn
ess
as C
aCO
3 58
8 =
N
one
0[6[
_000
6 25
/0[[/
2013
M
agne
sium
'
41
=
one
CC
GC
00
06
25/0
ct/2
013
Nitr
ate
+ N
itrite
as
N
53.9
N
one
I C
CG
C
0006
25
/Oct
/201
3 N
itrat
e as
NO
3_N
-
53.6
-
! N
one
0006
as
N
O2
'222
.2...
.2
222_
...
CC
GÇ
0006
25
/0[5
/201
3 N
itrite
as
NO
2 -N
0
3 _
. N
one
CC
GÇ
0006
25
/0ct
/201
3 P
otas
sium
6.
4 =
N
one
CC
GÇ
000
6 25
/Oó/
2013
S
od
m
131
=
None
0[6[_0006
25/0
ct/2
013
Spe
cific
Con
duct
ivity
15
43
=
Non
e
0[6[
_000
6 25
/Oct
/201
3 S
ulfa
te
229
=
Non
e
CC
GC
00
06
25/0[5/2013
Total D
isso
lved
Solids
1054
=
Non
e
'.r
CC
GC
000
7 21
/Oct
/201
3 A
lkal
inity
as
CaC
O3
135
=
Non
e
CC
GÇ
0007
21
/Oct
/201
3 B
icar
bona
te
165
=
`Non
e I_ C
CG
C _0
00]
21/0
[!/20
13
Cal
cium
44
=
None
0[6[_0007
21/O
ct/2
013
Chl
orid
e 71
=
N
one
CCGC_0007
21/Oct/2013
Har
dnes
s as CaCO3
180
=
None
006[
_000
] 21/Oct/2013
Magnesium
17
=
None
'
I C
CG
C 00
07
21/0
[!/20
13
Nitr
ate
+ N
itrite
as
N
11.6
6.:
=
Non
e
`[[6
[_ 00
07
I 21
/Oct
/201
3 N
itrat
e as
NO
3 -N
N
one
_.
-- _ -_
it
CC
GÇ
000]
21
/Oct
/201
3 N
itrite
as
NO
2 -N
02
=
N
one
i C
CG
C 00
07
21/O
ct/2
013
Pot
assi
um
2.4
=
Non
e
I
[CG
C 0
007
21/0
[5/2
013
Sod
ium
68
_
Non
e
0[6[
_000
7 21/Oct/2013
Spe
cific
Con
duct
ivity
688
=
i None
0o
0__,
C
CG
Ç 00
0]
21/Oct/2013
Sulfate
29
_
None
07
'CC
GC
_000
7 21
/Oct
/201
3 ;T
otal
Dis
solv
ed S
olid
s 431
_
Non
e
CC
GC
00
08
. 22
/Oct
/201
3 .
Alk
alin
ity a
s C
aCO
3 ¡
230
r
Non
e
1000
60
0008
22
/0cí
/201
3 I
Bic
arbo
nate
28
1 None
0[6[_0008
22 /Oct /2013
Calcium
218
_
None
[06[_0008
22/O
ct/2
013
Chl
orid
e 12
2 -
Non
e r :
CC
GC
_OO
118
22/O
ct/2
013
Har
dnes
s as CaCO3
775
None
CC
GC
00
08
22/O
ó/20
13
Mag
nesi
um
i 56
: C
CG
C_0
008
22/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
63
Non
e
Non
e C
CG
C
0008
22
/Oct
/201
3 N
itrat
s
NO
S-N
¡
62 J
a
I N
one
0222
__.
...
._.
-_ -.
. 22
22__
22
02._
C
CG
C
0008
22
/Oct
/201
3 N
itrite
as
NO
2 -N
0.
3 =
N
one
CC
GC
_000
8 22
/Oct
/201
3 P
otas
sium
6.
9 =
N
one
CC
GÇ
000
8 22
/Oó/
2013
S
odi
134
_
Non
e .
._._
._-
_'
0[6[
_000
8 22
/Oct
/201
3 S
pecr
ficC
ondu
ctvi
ty
1837
=
N
one
CC
GC
_000
8 22
/0ct
/201
3 S
ulfa
te
. 33
7 =
None
' CCGC0008
22/0
[5/2
013
Tot
al D
isso
lved
Sol
ids
1323
a
None
CC
GC
00
09
21/0Cí/2013
Alk
alin
ity as CaCO3
141
=
None
6[6[_0009
21/O
ct/2
013
Bia
rbon
ate
172
=
None
Nam
e Sa
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naly
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Res
ult
Res
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CC
GC
000
9 C
CG
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CC
GC
00
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CC
GÇ
0009
.. -
CC
GÇ
0009
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CG
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009
CC
GC
_000
9 C
CG
C
0009
CC
GÇ
0009
CC
GÇ
0009
CC
GC
000
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C_0
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CC
GC
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0
CC
GC
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C
WC
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Gr
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C
C- G
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10
CC
GC
_001
0 C
CG
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CC
GC
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0
CC
GC
_001
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CG
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010
__10
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CC
GC
_001
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CG
C
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11
CC
GC
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11
CC
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011
CC
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00
11
CC
GC
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CG
C
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CC
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CG
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12
CC
GC
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CG
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12
CC
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2 C
CG
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012
CC
GC
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2 C
CG
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012
CC
GC
001
2 C
CG
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012
CC
GC
_001
2 C
CG
C
0013
CC
GC
00
13
CC
GÇ
001
3
21/O
ct/2
013
21/0
Ct/2
013
1110
c./2
013
}-.2
013
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Cal
cium
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ate
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21
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itrite
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21
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15
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um
22.1
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Sodi
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21/C
m/2
013
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ate_
21
/Oct
/201
3 T
otal
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sel a
' sol
i&
25/O
ct/2
013
Alk
alin
ity a
s C
aCO
3 25
/Oct
/201
3 B
icar
bona
te
25/O
ct/2
013
Cal
cium
25/O
ct/2
013
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25/0
- t/2
013
Har
dnes
s as
Ca C
OE
25
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3 M
a
25/O
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013
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3 T
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21
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agne
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21
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/201
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tin__
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21/O
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013
21/O
ct/2
013
21/O
ct/2
013
Har
dnes
s as
CaC
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Mag
nesi
um
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itrite
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850
82
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3
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one
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e
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GC
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7
CC
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7
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013
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assi
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r
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17
CC
GC
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7
CC
GC
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7
CC
GC
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7
21/O
ct/2
013
Sod
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13
1 =
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one
21/0
ct/2
013
21/O
ct/2
013
21/O
ct/2
013
Spe
cific
Con
duct
ivity
,
2237
=
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one
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fate
T
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CC
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18
CC
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8
CC
GC
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18
CC
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00
18
CC
GC
00
18
CC
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8
CC
GC
00
18
CC
GC
_001
8
CC
GC
_001
8
CC
GC
00
18
21/O
ct/2
013
Alk
alin
ity a
s C
aCO
3 82
=
21/O
ct/2
013
21/O
ct/2
013
Bic
arbo
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cium
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0 14
50
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013
21/O
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ardn
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402
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21/O
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013
Mag
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itrite
as
N
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ate
as N
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N
40
: =
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one
78.2
78
i =
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one
=
1 N
one
21/O
ct/2
013
Nitr
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N
0.2
=
Non
e
21/O
ct/2
013
Pot
assi
um
2.5
=
Non
e
21/O
ct/2
013
Sod
ium
1
83
=
Non
e
21/O
ct/2
013
Spe
cific
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duct
ivity
12
38
' =
=
L N
one
' N
one
CC
GC
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8
CC
GC
00
18
21/O
ct/2
013
21/O
ct/2
013
Sul
fate
T
otal
D
isso
lved
Sol
ids
r
69
900
I =
N
one
CC
GC
00
19
24/O
ct/2
013
Alk
alin
ity a
s C
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3 13
7 =
N
one
CC
GC
00
19
CC
GC
00
19
CC
GC
00
19
CC
GC
00
19
24/O
ct/2
013
24/O
ct/2
013
Bic
arbo
nate
;
167
73
=
Non
e C
alci
um
=
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e
24/O
ct/2
013
24/O
ct/2
013
Chl
orid
e
256
=
Non
e H
ardn
ess
as C
aCO
3 =
N
one
CC
GC
_001
9 24
/Oct
/201
3 M
agne
sium
18
=
N
one
CC
GC
_001
.9
24/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
123
=
Non
e
CC
GC
_001
9
CC
GC
_001
9
24/O
ct/2
013
24/O
ct/2
013
Nitr
ate
as N
O3-
N
' 12
.2
=
Non
e N
itrite
as
NO
2-N
=
N
one
CC
GC
_001
9 24
/Oct
/201
3 P
otas
sium
2.
8 F
Non
e
CC
GC
00
19
CC
GC
_001
9
CC
GC
00
19
24/O
ct/2
013
24/0
a/20
13
Sod
ium
S
peci
ficC
ondu
ctiv
ity
.
22
572
. a
e
Non
e
24/O
ct/2
013
Sul
fate
86
=
N
CC
GC
00
19
CC
GC
00
20
CC
GC
_002
0
CC
GC
_002
0
CC
GC
_002
0
24/O
ct/2
013
21/O
ct/2
013
21/O
ct/2
013
21/O
ct/2
013
Tot
al D
isso
lved
Sol
ids
Alk
alin
ity a
s C
a C
O3
- ,
391
206
94
'
= =
Noo
nnee
N
Non
e c,
n e
Non
e
.i B
icar
bona
te
=
=
Cal
cium
21/O
ct/2
013
21/O
ct/2
013
Chl
orid
e ,
98
391
,a
Non
e
CC
GC
_002
0
CC
GC
_002
0
CC
GC
00
20
CC
GC
00
20
CC
GC
00
20
CC
GC
00
20
Har
dnes
s as
CaC
O3
a
N
e 21
/Oct
/201
3
21/O
ct/2
013
Mag
nesi
um
38
=
Non
e N
itrat
e-I-
Nitr
ite a
s N
.
Non
e
21/O
ct/2
01.3
N
itrat
e as
N
O3-
N
112-
i 1.
8 =
i
Non
e
21/O
ct/2
013
21/O
ct/2
013
Nitr
ite a
s N
O2-
N
Pot
assi
um
' 03
=
=
j Non
e
Non
e 3.
9 :
CC
GC
00
20
CC
GC
00
20
CC
GC
_002
0
21/O
ct/2
013
21/O
ct/2
013
Sod
ium
Spe
cific
Con
duct
ivity
!
70
1056
=
=
N
e N
one
21/O
ct/2
013
Sul
fate
14
5 =
N
one
CC
GC
00
20
CC
GC
00
21
CC
GC
00
21
CC
GC
00
21
21/O
ct/2
013
25/O
ct/2
013
Tot
al D
isso
lved
Sol
ids
5180
=
Non
e
Alk
alin
ity a
s C
aCO
3 16
9 '
=
Non
e
25/O
ct/2
013
25/O
ct/2
013
Bic
arbo
nate
C
alci
um
' t_
206
57
=
Non
e 1
=
Non
e
CC
GC
00
21
CC
GC
00
21
25/O
ct/2
013
25/O
ct/2
013
Chl
orid
e H
ardn
ess
as C
aCO
3
68
=
Non
e
208
=
Non
e
tts4-
0000
01 l,"
1^-s
taal
0701
41,4
4141
441/
4444
4 4
40
W:-
taaO
tTi l
a.,;;
"ike
iGkg
i C
CG
C
0021
25
/Oct
/201
3 M
agne
sium
16
=
CC
GC
00
21
25/O
ct/2
013
25/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
Nitr
ate
as N
O3-
N
Nitr
ite a
s N
O2-
N
: 3
: 0.
3
=
=
Non
e C
CG
C
0021
CC
GC
00
21
2-5/
Oct
/201
3 =
CC
GC
00
21
008C
_002
1 2-
5/O
ct/2
013
2-5/
Oct
/201
3
Pot
assi
um
= a
Non
e
Sod
ium
64
N
one
CC
GC
00
21
25/O
ct/2
013
Spe
cific
Con
duct
ivity
66
7 =
N
one
CC
GC
00
21
25/O
ct/2
013
Sul
fate
Tot
al D
isso
lved
Sol
ids
50
446
=
=
=
Non
e C
CG
C
0021
CC
GC
00
22
25/O
ct/2
013
25/O
ct/2
013
Alk
alin
ity a
s C
aCO
3 26
0 C
CG
C
0022
25
/Oct
/201
3 B
icar
bona
te
317
=
o: nn
n ee
e N
one
CC
GC
00
22
25/O
ct/2
013
Cal
cium
20
9 =
N
one
CC
GC
00
22
25/O
ct/2
013
Chl
orid
e 36
0 e
Non
e
o
CC
GC
00
22
CC
GC
00
22
CC
GC
00
22
CC
GC
00
22
H C
CG
C
0022
CC
GC
00
22
25/O
ct/2
013
25/O
ct/2
013
2S/O
ct/2
013
25/O
ct/2
013
25/O
ct/2
013
25/O
ct/2
013
Har
dnes
s as
C
aCO
3
Mag
nesi
um
Nitr
ate
+ N
itrite
as
N
: N
itrat
e as
NO
3-N
892
90
71.7
71.5
= e =
- - N
one
=
inn
Non
e N
itrite
as
NO
2-N
0.
2 =
NN
N
Pot
assi
um
211
2457
,
= a =
a.
Non
e
CC
GC
00
22
'- C
C-G
C
0022
I
25/O
ct/2
013
25/0
c4/2
013
Sod
ium
S
peci
ficC
ondu
ctiv
ity
Sul
fate
Non
e
' Non
e C
CG
C
0022
25
/Oct
/201
.3
CC
GC
_002
2 25
/Oct
/201
3 T
otal
Dis
solv
ed S
olid
s
1250
754
i 16
3
=
=
nnn
Non
e
Non
e C
CG
C
0023
21
/Oct
/201
3 A
lkal
inity
as
CaC
O3
CC
GC
00
23
21/O
ct/2
013
Bic
arbo
nate
19
9 =
N
one
CC
GC
00
23
CC
GC
002
3 21
/Ott/
2013
21
/Oct
/201
3 C
alci
um
Chl
orid
e 63
53
= ,
Non
e
nnn e
ee
Non
e
I C
CG
C 00
23
CC
GC
00
23
21/O
ct/2
013
21/O
ct/2
013
Har
dnes
s as
CaC
O3
Mag
nesi
um
252
23
=
=
CC
GC
00
23
CC
GC
00
23
21/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
' N
itrat
e as
NO
S-N
1.5
=
21/O
ct/2
013
1 2
=
CC
GC
002
3 21
/Oct
/201
3 :
21/O
ct/2
013
21/O
ct/2
013
Nitr
ite a
s N
O2-
N
Pot
assi
um
Sod
ium
0.3
3.6
'
50
720
'
120
= . =
=
=
----
"
eee
Non
e N
one
Non
e
'
r C
CG
C 00
23
CC
GC
00
23
I C
CG
C 00
23
21/O
ct/2
013
Spe
cific
Con
duct
Nity
N
one
CC
GC
00
23
21/O
ct/2
013
Sul
fate
N
one
CC
GC
00
23
21/O
ct/2
013
Tot
al D
isso
lved
Sol
ids
463
=
Non
e
CC
GC
00
24
24/O
ct/2
013
Alk
alin
ity a
s C
aCO
3 -
166
1 =
.
' -
CC
GC
D
024
CC
GC
00
24
CC
GC
00
24
CC
GC
00
24
24/O
ct/2
013
' 24
/Oct
/201
3
24/O
ct/2
013
24/0
c1/2
013
Bic
arbo
nate
C
alci
um
Chl
orid
e H
ardn
ess
as C
aCO
3
: 20
3
224
=
- =
a
Non
e -N
one-
C
CG
C
0024
24
/Oct
/201
3 M
agne
sium
;
18
: =
N
one
CC
GC
00
24
24/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
; 18
'
1.5
=
: =
Non
e
CC
-GC
00
24
24/O
ct/2
013
Nitr
ate
as N
O3-
N
CC
GC
00
24
24/O
ct/2
013
Nitr
ite a
s N
O2-
N
, 0.
3 -
a a C
CG
C
0024
CC
GC
00
24
24/O
ct/2
013
24/O
ct/2
013
Pot
assi
um
Sod
ium
'
- 35
=
CC
GC
00
24
24/O
ct/2
013
Spe
cific
Con
duct
ivity
'
551
76
- =
a o:
nnn
eee
Non
e
Non
e C
CG
C
0024
24
/Oct
/201
3 S
ulfa
te
CC
GC
00
24
24/O
ct/2
013
Tot
al D
isso
lved
Sol
ids
371
=
CC
GC
00
25
L
CC
GC
002
5 24
/Oct
/201
3 '
24/O
ct/2
013
Alk
alin
ity a
s C
aCO
3
Bic
arbo
nate
224
i 27
3
= e
Non
e .
Non
e
CC
GC
00
25
24/O
ct/2
013
Cal
cium
:
101
=
CC
GC
00
25
24/O
ct/2
013
, C
hlor
ide
42
: a
Non
e
CC
GC
00
25
24/O
ct/2
013
Har
dnes
s as
CaC
O3
372
= =
IINN
Non
e
CC
GC
00
25
24/O
ct/2
013
Mag
nesi
um
29
Non
e
.
=el
o=ci
r N
ame
sam
pleD
ate
3lyt
eNam
e C
CG
Ç 0
025
CC
GC
.002
5 C
CG
C_0
025
CC
GC
0025
CC
GC
_002
5
CC
GÇ
0025
C
CG
C_0
025
CC
GC
_
CC
GC
_ '<
C
CG
C_0
026
CC
GC
_002
6 C
CG
C00
26
CC
GC
_002
6 C
CG
Ç 00
26
CC
GC
_002
6 C
CG
C_0
026
----
- __
26
C =126
CC
GC
00
26
CC
GC
_002
6
CC
GC
_002
6 CCGC_0Ó26
_?s2
7 _ S27
006[
_002
7 C
CG
C_0
027
CC
GC
_002
7
CC
GC
_002
7 C
CG
C_0
027
CC
GC
_002
7 C
CG
Ç 00
27
CC
GC
_002
7 C
CG
C 0
027
CC
GC
_002
7
CC
GC
_002
7 C
CG
C_0
028
CC
GÇ
_002
8 C
CG
C_0
028
CC
GC
002
8
CC
GC
_002
8
CC
GC
_002
8 C
CG
C_0
028
CC
GC
_002
8
CC
GC
_00 2
8 C
CG
C 0
028
CC
GÇ
0028
C
CG
C_0
028
CC
GÇ
0028
CC
GC
_002
8 C
CG
C_0
0'S
CC
GC
o-P
C
CG
C_0
03
CC
GC
00_
CC
GC
_00_
. C
CG
C
002-
CC
GC
_002
S
24/0
e/20
13
24/0
[[/2
013
24/á
t/201
3 24
/áf/
2013
24
/Oct
/201
3 24
/át/2
013
24/0
0[/2
013
24/á
t/201
3 24
/át/2
013
24/á
t/201
3 24
/Oct
/201
3 24
/át/2
013
24/á
/201
3 24
/Oct
/201
3
24/O
ct/2
013
24/O
ct/2
013
24/O
ct/2
013
24/O
ct/2
013
24/0
d/20
13
24/O
ct/2
013
24/0
0[/2
2013
Nitr
ate
+ N
itrite
as
N.
Nitr
ate
as N
O3-
N
Pota
ss _
97
F=_
3 !-
0rw
ivs_
_
C a Ha r
dnes
s as
Ca_
_-
Mag
nesr
m
Nitr
ate
+S
-=_
+:
Nitr
ate
.s22
,2_
., as
r: a
s T.=
_'{
Sodi
um
Spec
ific
Co-
_niv
-
Si. f
ace
T
_ D
'ese
ued
Soli-
=
A
nay
as C
2CO
3
B ic
arbo
nate
C
alci
um
24/O
ct/2
013
24/O
ct/2
013
NI-
=
',tnt
easN
24
/Oct
/201
3 N
7tm
ce a
s '4
03-9
24
/á0J
2013
N
itrite
as
N _2
-+J
_._
-233
Po
bssi
um
IC
q,-r
- 01
3 I_
5aoi
um
/231
3 sp
ecif
icC
onar
_.ar
. Sc
Cm
te
4/ca
/201
.E.
24;'O
2'20
13
Alk
alin
ity a
sC=
ï - `
24/0
t/201
3 B
icar
bona
te
24/O
ct/2
9=
l_--
24
/Oct
/2"1
...
_
24/á
t/201
3 =
-_
_ _
_ __
_,
_ _
24/0
ct/2
013
Mag
nesi
um
24/0
ct/2
013
Nitr
ate
+ N
itrite
as
N
24/á
t/27.
:-
S -
as -
,M.,-
4
24/á
t/203
3 P_
c =ac
n --
24/O
ct/2
013
-24/
0e/2
013
Spen
fieÇ
. nd
-_,-
. 24
/Oct
/201
3 Su
lfat
e
2424
-/20
13
Tot
al D
isso
lved
Sol
ids
lclin
ity a
s C
aCO
3 - c
_
a:7-
-"::a
te
24/á
t/201
_
3 O
s
24/0
e/20
13
-
Chl
,n_
__
24/O
ct/2
013
He
-
- ss
as
=_O
3 24
/Oct
/201
3 M
agne
sium
2
-C
Nitr
ate
+N
i -a
3.8
793
Se
193
13
2.7
N-n
=
Noc
e
Non
e er
e
Ncr
e SJ
-.-
[{-,
a
Nos
e N
ose
zore
ttrne
mor
e
honeRog=
ac -e
Non
_
hole
N
die
"t re
\o
re
Not
e
ns
hose
NC
_-_
Non
e N
one
Nitr
e
iéld
Pdvi
ut
.;
mpl
éÜ
Näm
é:'
Res
Qua
l
oAëd
de
9--2
c 09
20
C00
C 0
029
CC
GC
_002
9 C
CG
C
0029
C 0
029
0000
0030
24
L-2
`5
Alk
alin
ity =
s C
a___
_c
_ 00
30
24/0
e/20
13
Nitr
ate
as N
O3-
N
24/O
ct/2
013
Nitr
ite a
s N
O2 -
N
24/0
=12
:13
Fflu
it:
24 /O
t +z=
4
CC
GÇ
0030
CC
GC
r003
0-
LW
C
- __
_
CC
GC
__
_
CC
Oç 005r
CC
GC
=
cC
GC
t3
3r
CC
GC
____
_ C
CG
C_G
'__
CC
GC
003
0
_ 3
Har
dnes
s -s
- r
3C_5
_ 20
13
Nitr
ate
+ N
itrite
as?
. '
-- _0
13
Nitr
ate
as N
O3-
N
' .1
2013
=
c=.-
_ 24
/Oct
/201
3 Sp
ecfi
_.--.
24/0
Ct/2
013
Sulf
ate
24/
__
___
_-
o
...-_
__
CC
GC
_003
1 22
20
13
Bia
roc-
-re
CC
GC
00
31
- _
_201
3 C
alci
um
"_--
... -
_ ...
C
CG
C 0
031
2_ _
20
13
" _
_ C
G_ 0
031
__
013
--
as W
C_'
_ ".
___ _
..__.
_..
.-...
_.
._
--
CC
GÇ
003
1
-CG
C CrE:
CC
GC
0031
CC
GC
_003
1 C
CG
C_0
031
CC
GC
003
1
CC
GÇ
003
1 C
CG
C
0031
0000
.0ó3
z
CC
GÇ
0032
C
CG
C
0032
C
CG
C
0032
C
CG
C 0
032
CC
GC
003
2
22/0
0/20
13
Nitr
ite a
s N
O2 -
N
22/0
0/20
13
Pota
ssiu
m
2013
So
dium
22 - -2013
Spe
nfi
X20
13
Sulf
ate
22/O
ct/2
013
Tot
al D
isso
lved
So:
os
as
25/á
t/201
3 -
Alk
ahn
. as
CaC
OS
25/O
Ct/2
013
Chl
orid
e
25/á
í/z01
3 H
ardn
ess
=02
3
Mag
nesi
um
Nitr
ate
+ N
itrite
es
7.
3 N
itrat
e as
NO
S -N
25/O
ct/2
013
Nitr
ite as
NO
2 -N
2 25
/0C
í/201
3 Po
tass
ium
0 00
32
CC
GC
-'_
_ C
CG
C
CC
GC
CC
-39,
_ i_
-_
CC
GC
_003
3 C
CG
C_0
033
CC
GC
00
33
2013
T
otal
Dis
solv
ed S
c -.
ts
22/0
Ct/2
013
_za
22/a
-_-.
/2-9
:9
-__-
__
..
22/O
_-
-__
=-
=
22/
- _
- 22
/0S/
2013
.._
__M
agne
s
- -
22/O
ct/2
013
Nitr
ate+
^.-=
_Y
_
_-20
13
Nitr
ate
as N
O3-
N
2.4
0.3
429
67
667
92
1494
34
2
1094
32
8
175
1090
1488
308
37e
2.3
Non
Non
e
Non
e N
one
Non
e N
one
Non
e
None
Non
e N
one
Non
e
Non
e
Non
e N
one
Non
e N
one
Non
e __
Non
e
zone
'.one
Non
e
dx,
á
I((
..
Ì I
I
I
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_L6
CC
GC
00
56
CC
GC
0056
C
CG
C 0
056
CC
GC
_005
6
CC
GC
00
56
CC
GC
00
56
CC
GC
00
56
CC
GC
_005
6
CC
GC
_005
6
CC
GC
_W56
CC
GC
_005
6
CC
GC
0356
C
CG
C
00$6
_
___6
CC
GC
00
56
CC
GC
0D56
CC
GC
_W56
CC
GC
0056
CC
GC
_005
6
CC
GC
_005
6
CC
GC
_005
6
CC
GC
_00
=
CC
GC
-
_00
CC
GC
0056
C
CG
C
0056
C
CG
C_0
056
CC
GC
0056
CC
GÇ
005
6
CC
GC
_005
6
CC
GC
_005
6
CC
GC
00
5-
CC
GC
-56
C
CG
C 00
56
CC
GC
_005
6
CC
GC
_00_
_
CC
GC
_4
C
CG
C
00=
=
CC
GC
_005
6
CC
GC
0056
C
CG
C 00_.
CC
GC
_00_
-
CC
GC
035
6 C
CG
_C_W
56
CC
GC
-005
6
CC
GC
_005
6
CC
GC
035
6 C
CG
C 00
56
CC
GC
0056
C
CG
C00
56
CC
GC
00
56
CC
GC
005
6 C
CG
C 0
056
CC
GC
_W__
CCGÇ 00
5=
CC
GC
03
55
-_01
4 ...
Z
S/C
c/20
1i
_.
!vm
_
_ C
i.lor
ide
CI -
ride
28/A
ug/2
014
,_
28/A
ug/2
014
- _
-28/
Aug
/201
4 .-
ss
a ..
.
23JO
Cí/2
013
Har
dnes
as
Ca
CO
3
23/O
ct/2
013
Har
dnes
as
u_-
23/O
ct/2
013
Har
dnes
s as
28/A
ug/2
014
Har
dnes
s -C
a¡_
28/A
ug23
1_
._
essa
_ C
aCO
3
28/A
ug/Z
S: 4
H
a-tr
ess
as C
a003
23
/Oct
/2C
5 -
- -
23/O
ct/2
Ca
...
_
23/0
ct/2
0-
:agn
es
..
28/A
ug/2
al
--
g -
28/A
ug)2
__
'Fag
nesi
u-
28/A
ug/2
014
Mag
nesi
um
23/0
.-t/2
013
Nitr
ate
+ N
itrite
as
N
23/O
ct/2
013
23/O
ct/2
013
N
-= '
28/A
ug/2
014
Nitr
ate
+ N
itrite
asN
28
/Aug
/201
4 N
itrat
e +
Nitr
ite a
s N
28/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
=/O
ct/2
013
Nitr
ate
as NO3-N..
3/O
tt/20
13
Nitr
ate
as N
O3
N
Fël
dpoi
nt
Namér
CC
GC
_005
9 23
/Oct
/201
3 N
itrite
as
NO
2 -N
0.
4 _
! N
one
CC
GC
_005
9 28
/Aug
/201
4 N
itrite
as
NM
-N
0.4
Non
e _
CC
GC
_005
9 23
/Oct
/201
3 P
otas
sium
3.
6 00
0-
Non
e
CC
GC
_005
9 28
/Aug
/201
4 P
otas
sium
3.
5 =
D
CC
GC
_005
9 23
/Oct
/201
3 S
odiu
m
84
=
Non
e
CC
GC
_00S
9 28
/Aug
/201
4 S
odiu
m
88
=
0060
_005
9 23
/Oct
/201
3 S
peci
ficC
ondu
ctiv
ity
1172
=
N
one
'
CC
GC
_005
9 28
/Aug
/201
4 S
peci
ficC
ondu
ctiv
ity
1311
N
one
CC
GC
_005
9 23
/Oct
/201
3 S
ulfa
te
259
=
Non
e
CC
GC
_005
9 28
/Aug
/201
4 S
ulfa
te
280
=
Non
e
CC
GC
0059
23
/00/
2013
T
otal
Dis
solv
ed S
olid
s 81
7 =
N
one
CC
GC
_005
9 28
/Aug
/201
4 T
otal
Dis
solv
ed S
olid
s 91
7 =
N
one
CC
GC
006
0 21
/Oct
/201
3 A
lkal
inity
as
CaC
O3
19]
=
Non
e
CC
GC
00
60
21/O
ct/2
013
Bic
arbo
nate
24
0 N
one
0060
_006
0 21
/Oct
/201
3 C
alci
um
72
=
Non
e
0060
_006
0 21
/Oc/
2013
C
hlor
ide
22
Non
e
CC
GC
00
60
21/O
ct/2
013
Har
dnes
s as
CaC
O3
270
=
I N
one
CC
GC
_006
0 21
/Oct
/201
3 M
agne
sium
22
=
1
Non
e
CC
GC
_006
0 21
/Oct
/201
3 I
Nitr
ate
+ N
itrite
as
N
0.5
=
Non
e
CC
GC
_006
0 21
/Oct
/201
3 N
itrat
e as
NO
S -N
0.
3 =
N
one
0060
_006
0 21
/0C
í/201
3 N
itrite
as
NO
2 -N
0.
4 _
Non
e
0060
_006
0 21
/00/
2013
P
otas
sium
2.
6 =
N
one
0060
_006
0 21
/Oct
/201
3 S
odiu
m
30
_ -:
Non
e
0060
_006
0 21
/Oct
/201
3 S
peci
ficC
ondu
ctiv
ity
622
=
Non
e ,
CC
GC
_006
0 21
/00/
2013
S
ulfa
te
98
=
None
CC
GC
_006
0 C
CG
C 00
61
21/O
ct/2
013
23/O
ct/2
013
Tot
al D
isso
lved
Sol
ids
409
207
_ N
one
Non
e A
llcal
inity
as
CaC
O3
23/O
ct/2
013
Bic
arbo
nate
None
CCGC_0061
23/Oct/2013
Calcium
276
=
Non
e
CC
GC
_006
1 23
/Oct
/201
3 C
hlor
ide
246
=
I N
one
0060
_006
1 23
/00/
2013
H
ardn
ess
as C
aCO
3 99
0 _
' N
one
0060
_006
1 23
/Oct
/201
3 M
agne
sium
73
-
' _
' N
one
CC
GC
_006
1 23
/Oct
/201
3 N
itrat
e +
Nitr
ite a
s N
53
.8
i N
one
CC
GC
_006
1 23
/00/
2013
'
Nitr
ate
as N
O3
-N
53.6
N
one
CC
GC
00
61
23/O
ct/2
013
Nitr
ite a
s N
O2 -
N
0.2
=
' N
one
CC
GC
00
61
23/0
0/20
13
Pot
assi
um
6.3
_ N
one
CC
GC
_006
1 23
/Oct
/201
3 S
odiu
m
92
_
Non
e
CC
GC
_006
1 23
/Oct
/201
3 S
peci
ficC
ondu
ctiv
ity
2087
_
Non
e
CC
GC
_006
1 23
/O0/
2013
S
ulfa
te
365
Non
e
CC
GC
00
61
23/0
0/20
13
Tot
al D
isso
lved
Sol
ids
1503
-
Non
e
CC
GC
006
2 23
/Oct
/201
3 '
Alk
alin
ity a
s C
aCO
3 14
1 N
one
CC
GC
_006
2 23
/Oct
/201
3 B
icar
bona
te
172
=
Non
e
CCGC_0062
23/Oct/2013
Calcium
49
Non
e
CC
GC
_006
2 23
/Oct
/201
3 C
hlor
ide
19
_ ¡
None
CC
GC
00
62
23/O
ct/2
013
Har
dnes
s as
CaC
O3
201
_ N
one
CC
GC
_006
2 23
/00/
2013
M
agne
sium
19
=
N
one
CC
GC
00
62
23/0
0/20
13
Nitr
ate
+ N
itrite
as
N
1.3
=
F
Non
e J
CC
GC
_006
2 23
/Oct
/201
3 N
itrat
e as
NO
3 -N
1
=
Non
e
CC
GC
_006
2 23
/Oct
/201
3 N
itrite
as
NO
2 -N
03
-
None_
CC
GC
00
62
23/0
0/20
13
Pot
assi
um
15
I Non
e
CC
GC
00
62
23/0
Cí/2
013
Sod
ium
28
=
I
Non
e
CC
GC
00
62
23/O
0/20
13
Spe
cific
Con
duct
ivity
48
1 =
N
one
CC
GC
00
62
23/O
ct/2
013
Sul
fate
69
=
N
one
CC
GC
_006
2 23
/00/
2013
T
otal
Dis
solv
ed S
olid
s 1
308
=
Non
e
CC
GC
006
3 23
/00/
2013
A
lkal
inity
as
CaC
O3
' 20
2 N
one
CC
GC
00
63
23/Oct/2013
Bicarbonaté
246
Non
e
CC
GC
00
63
23/O
ct/2
013
Cal
cium
22
1 N
one
P7
i C
CG
Ç 00
63
23 /O
ct /2
013
Chl
orid
e I
178
=
Non
e
CC
GC
_006
3 23
/001
2013
H
ardn
ess
as C
aCO
3 72
1 =
N
one
CC
GC
00
63
23/0
cí/2
013
Mag
nesi
um
41
=
Non
e
CC
GC
00
63
23/O
ct/2
013
Nitr
ate
+ N
itrite
as
N
25.7
=
N
one
-
CC
GC
_006
3 23
/Oc/
2013
N
itrat
e as
N
O3
-N
25.5
-
Non
e 3
.-
Non
e _
CC
GC
00
63
23/0
0120
13
Nitr
ite as
N
O2
-N
0.2
=
Non
e
CC
GC
006
3 23
/00/
2013
P
otas
sium
63
-
. N
one
. _
-_
CC
GÇ
0063
23
/00/
2013
S
odiu
m
99
e None___
CC
GC
0063
23
/00/
2013
S
peci
ficC
ondu
ctiv
ity
1653
_
__N
one_
___
CC
GC
00
63
23/0
0/20
13
Sul
fate
31
2 =
N
one
006[
_006
3 23
/Oct
/201
3 T
otal
Dis
solv
ed S
olid
s 1
1137
e
Non
e
CC
GC
00
64
22/0
0/20
13
Alk
alin
ity a
s C
aCO
3 15
0 =
N
one
0060
_006
4 22
/00/
2013
B
icar
bona
te
183
=
Non
e
CC
GC
00
64
22/0
0/20
13
Cal
cium
49
-
Non
e
0060
0064
22
/Oct
/201
3 C
hlor
ide
20
e r
Non
e
CC
GC
00
64
22/0
0/20
13
Har
dnes
s as
CaC
O3
209
=
Non
e _.
. .._
......
i-
CC
GC
00
64
22/0
0/20
13
Mag
nesi
um
21
=
Non
e
CC
GC
00
64
22/0
0/20
13
Nitr
ate
Nitr
ite a
s N
3
- N
one .
- - -
.. 00
60_0
064
22/0
0/20
13
Nitr
ate
as
NO
3 -N
2 ]
=
Non
e
CC
GC
00
64
_ 22
/Oct
/201
3 N
itrite
s N
O2 -
N
03
=
Non
e 30
00_-
C
CG
C
m
1.4
0064
22
/00/
2013
P
otas
siu
=
Non
e -.
._
CC
GÇ
0064
- - 22
/OC
í/201
3 S
odiu
m
30
=
Non
e e
0060
_006
4 22
/Oct
/201
3 S
peci
ficC
ondu
ctiv
ity
519
=
I N
one
CC
GC
_006
4 22
/00/
2013
S
ulfa
te
74
=
Non
e
CC
GC
00
64
22/0
0/20
13
".
Tot
al D
isso
lved
Sol
ids
371
=
_-
,_N
one
CC
GC
006
5 22
/00/
2013
A
lkal
inity
as
CaC
O3
316
- N
one
-___
- _.
_.
-__
CC
GC
00
65
22 /O
ct /2
013
T B
icar
bona
te
386
=
Non
e
CC
GC
00
65
22/0
0/20
13
Cal
cium
20
1 =
N
one
0060
_006
5 22
/0C
í/201
3 C
hlor
ide
132
None
. -.
__
3030
-_
CC
GC
00
65
22/0
0120
13
Har
dnes
s as
CaC
O3
-
910
_ N
one
CC
GC
_006
5_
-- 22
/00/
2013
M
agne
sium
_0
303
99
=
Non
e
, C
CG
C_0
065
22/O
ct/2
013
Nitr
ate
+N
itrite
as
N
14.2
=
:
Non
e
CC
GC
00
65
22/0
0/20
15
Nitr
ate
as N
O3
-N
13.8
=
N
one
CC
GC
00
65
22/0
0/20
13
' N
itrite
as
NO
2 -N
0.
4 =
I
Non
e
CC
GC
00
65
22/0
0/20
13
Pot
assi
um
4.7
:
=
Non
e
0060
_006
65
22/0
0120
13
Sod
ium
i
191
=
Non
e
CC
GC
006
5 22
/Oct
/201
3 S
peci
ficC
ondu
ctiv
ity
2161
e
Non
e
CC
GC
.006
5 22/0 12013
Sulfate
659
=
None
0330
_.
__. --
C
CG
C 00
65
` 22
/Oct
/201
3 T
otal
Dis
solv
ed S
olid
s 16
74
=
Non
e
CC
GC
00
66
22/0
0/20
13
Alk
alin
ity a
s C
aCO
3 24
7 =
N
one
.
CC
GC
00
666
22/0
0/20
13
Bic
arbo
nate
30
1 =
N
one
CC
GC
00
66
22/0
0/20
13
Cal
cium
82
e
Non
e
I CCGC_0066
22/O
ct/2
013
Chloride
_ 62
=
None
CC
GC
22
/00/
2013
H
ardn
ess
as C
aCO
3
_378
, _
Non
e
CC
GÇ
0066
22
/00/
2013
M
agne
sium
42
_
Non
e
0060
_006
6 22
/0C
í/201
3:
Nilr
ate
+N
itrite
as
N
4.8
=
Non
e
0060
_006
6 .
22/0
0/20
13_
Nitr
ate
as
NO
3 -N
4.
5 e
Non
e
CC
GC
_006
6 22
/00/
2015
N
itrite
as
NO
2 -N
03
=
N
one
CC
0000
66
22/0
0/20
13
Pot
assi
um
23
=
Non
e 00
C
CG
C
0066
22
/00/
2013
S
odiu
m
-
100
=
Non
e
CC
GC
00
66
22/0
a/20
13
Spe
cific
Con
duct
ivity
10
60
_ N
one
CC
GC
00
66
22/0
0/20
13
Sul
fate
20
8 -
None
0060
_006
6 22
/00/
2013
T
otal
Dis
solv
ed S
olid
s 70
8 _
Non
e
0060_0067
-
25/00[/2013
Alk
alin
ity as CaCO3
192
_
None
0060_0067
25/Oct/2013
'
Bicarbonate
234
_
Non
e
CC
GC
_006
7 25
/002
013
Cal
cium
=
None
.
-
CC
GC
00
67
25/0
0/20
13
Chl
orid
e 28
_
Non
e
sL'=
o-.
tme
Sam
pleD
ate
CC
GC
_006
7
CC
GC
_006
] C
CG
Ç 00
67
CC
GC
_006
7 C
CG
C_-
o C
CG
C a
_cv
CC
GÇ
0067
C
CG
C_0
067
CC
GC
00
67
CC
GÇ
006
8
CC
GC
_006
8 C
CG
C
0068
CC
GC
_006
8
CC
GÇ
0068
CC
GC
_006
8 C
CG
C_0
068
CC
GÇ
0068
C
CG
C 0
068
CC
GC
_006
8 W
C 0
068
CC
GC
_006
8 C
CG
C_0
068
CC
GC
_006
8 C
CG
C00
69
CC
GÇ
006
9
CC
GÇ
0069
CCGC21069-
CC
GC
_006
9 C
CG
Ç 00
69
CC
GC
.006
9 C
CG
C_W
69
CC
GC
_006
9 C
CG
Ç 00
69
CC
GC
_006
9 C
CG
C00
69
CC
GC
006
9
CC
GC
00
69
CC
GC
_006
9 C
CG
C_0
069
CC
GÇ
0069
C
CG
C
0069
CC
GC
0069
CC
GC
_006
9 C
fyC
006
9 C
CG
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7 10
/Mar
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10 /M
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10
/Mar
/201
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01
07
10 /M
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107
10 /M
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014.
H
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GC
01
07
10 /M
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7727
0307
10
/Mar
/201
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07
10 /M
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01
07
10 /M
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014
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10 /M
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07
10/M
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CC
GC
01
07
10 /M
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014
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10
/Mar
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10
/Mar
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08
10 /M
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014
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01
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10 /M
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014
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cium
7727
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8 10
/Mar
/201
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CC
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01
08
10 /M
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014
Har
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201
4 M
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8 10
/Mar
/201
4 P
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10
/Mar
/201
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10 /M
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014
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cifle
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GC
01
08
10 /M
ar /2
014
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C
CG
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08
10/M
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014
Tot
al D
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lved
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CC
GC
01
09
10 /M
ar /2
014
Alk
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ity as
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01
09
30 /M
ar /2
014
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arbo
nate
CC
GC
01
09
10 /M
ar /2
014
Cal
cium
CC
GC
01
09
10 /M
ar /2
014
Chl
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CC
GC
01
09
10 /M
ar /2
031
Har
dnes
s as
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CC
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0109
10
/Mar
/201
4 M
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27_0
109
10 /M
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014
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GC
01
09
10 /M
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014
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GC
01
09
10 /M
ar /2
014
Nitr
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7727
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9 10
/Mar
/201
4 P
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2.
6 e
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01
09
10 /M
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014
í S
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m
34
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GC
01
09
10/M
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014
Spe
cific
Con
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47
4 e
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GC
01
09
10 /M
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014
Sul
fate
72
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GC
01
09
- 10
/Mar
/201
4 T
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solv
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s 32
6 e
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CC
GC
01
10
10 /M
ar /2
014
Alk
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CO
3 30
1 _
Non
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CC
GC
01
10
10 /M
ar /2
014
- B
icar
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367
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GC
01
10
10 /M
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014
Cal
cium
r
230
e D
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GC
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0 10
/Mar
/201
4 C
hlor
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178
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10
/Mar
/201
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10
/Mar
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Mag
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0 C
CG
Ç
Ç 03
30
10 /M
ar /2
014
Nitr
ate
+ N
itrite
as
N
0.2
=
Non
e
CC
GC
01
10
10 /M
ar /2
014
Nitr
ate
as N
O3
-N
=.1
=
N
one
= e -
Non
e
Non
e
Non
e
_ -c
= ç .5
=
1
Non
e
_'-
=
197
_ '.o
ne
1094
128
e N
one
156
Non
e
- 12
7 ~
e
D
211
e N
one
609
-
_ eise
73
e -
_ _
e _
e I
D
S'_
?3
D
2205
N
one
297
- N
one
1503
e
l N
one
231
=
Non
e 28
2 e
%on
e
69
: e
180
=
one
267
Non
e
23
_ D
_._
_ e
_.-
_ :o
ne
<0.
1 -N
D
Non
e 4.
3 _
=1
_ _
- -
5 e
Non
e
ee
e
Non
e
626
e N
one
152
i e
Non
e
5-
_ _
"-
ire
Äïia
lyte
Nam
e
CC
GC
_011
0 C
CG
C
0110
CC
GC
_011
0 C
CG
C
0110
CCGC_0110
CC
GC
_011
1
cCG
C_0
111
CC
GC
_011
1 C
CG
C_0
111
CC
GC
011
1 C
CG
C01
11
CC
GC
_011
1 C
C-G
C Ç
0111
CC
GÇ
011
1
CC
GC
_011
1 C
CG
C 0
111
ÇC
GC
01
11
CC
GC
_011
1 C
CG
C-0
331
CC
GC
_011
2 C
CG
C01
12
CC
GC
_011
2 C
CG
Ç 01
12
CC
GC
011
2 C
CG
C
0112
CC
GÇ
0112
CC
GC
_011
2
CC
GC
_011
2 C
CG
C_0
112
CC
GC
01
12
CC
GC
_011
2 C
CG
C_0
112
CC
GC
01
12
CC
GC
_011
3 C
CG
C
0113
CC
GC
_011
3 C
CG
C 0
113
CC
GC
_011
3 C
CG
C_0
113
ttbC
_011
3 C
CG
C
0113
CC
GC
01
13
CC
GC
_011
3 C
CG
C
0113
CC
GC
011
3
CC
GC
_011
3 C
CG
C
0113
C
CG
C
0114
CC
GÇ
0114
CC
9C01
14
CC
GC
011
4
CC
GÇ
0114
C
CG
C
0114
C
CG
C 0
1='
CW
C_ W
"-
CC
GC
_011
=
101M
a120
14
Nitr
ite a
s NO
2 -N
10
/Mar
/201
4 Po
tass
ium
10/M
ar/2
014
Sodi
um
10/M
ar/2
014
SPA
., fi
C- _
_ -
ST:
10 M
ar L
0í4
Sulf
ate
I D
sso
orac
i ac
ilk
m
y - A
CT
_ 10
/Man
201=
B
ali-
cram
10
/Mar
-`0'
C
alca
m
10/M
ar/2
0144
C
hlor
ide
10 /M
ar /2
014.
H
ardn
ess
as S
a-ú=
10
/ /Mar
/201
4 M
agne
síur
10
/Mar
/201
4 N
itrat
e +
Nitr
ite a
s N
10/M
ar/2
014
Nitr
ate
as N
O3
-N
10/M
ar/2
014
Nitr
ite a
s 14
02-N
10
/Mar
/201
4 Po
tass
ium
10
/Mar
/201
4 __
_.
10/M
ar/2
014
S -.
-Car
ta
10/M
ar /2
014
Su a
te
10/M
ar/2
014
Tot
al D
isso
lved
Sol
:==
10/M
ar/2
014
Alk
alim
:a
s Caa
ai
10 /M
ar /2
014
Bic
arbo
nate
10
/Mer
/201
4 C
alci
um
10/M
er23
14
10/M
ar/2
C_
_ --
_
a-Z
CS
1O /M
a :/2
014
Mag
nesi
um
10/M
ar/2
014
Nitr
ate
+`a
r. -:
teas
af
10/M
ar/2
014
Nitr
ate
as
_3N
10
/Mar
/201
4 N
itrite
as
,-;
10/M
ar/2
014
Poca
ssi=
a 10
/Mar
/201
4 --
_
10 /M
a /<
14
5 v
16/M
arl2
C14
-
tate
0/M
ar/2
P14.
-s
tai
Las
axer
Sca
ds.
_
11/M
ar/2
014
Alk
alin
ity =
as _
- 11
/Mar
/201
4 B
icar
bona
te
-
11 /M
ar12
C14
'_ =,
rr
-
_
11/M
ar/2
G4
11/M
ar/ -
C4
-a-
-ec
as C
a:: -
_ 11
/Mar
/201
4 M
agne
siu
--
11 /M
ar /2
014.
N
itrat
e +
Y:
as
11/M
er/2
014
Moa
te e
s 3.
11
/Mar
/201
4 N
i -
';C:-
1--;
11/M
ar/2
014
Pota
ssiu
m
11 /M
ar/2
014
Sodi
um
11/M
er/2
014
spen
ficC
o.._
-.
.. i
11/M
ar/2
014
Sulf
ate
11/M
er/2
014
Tot
al D
isso
l. =So
lid_
11 /M
ar/2
014
Alk
alin
ity as
CaC
O3
11/M
ar /2
014
-
Bic
arbo
nate
11
/Mar
2_4
lanr
11
/Ma
/2'_
C
rac-
ca
11/M
ar/2
2 re
dnes
s as
11/M
ar/2
014
Mag
nesi
um _
1/M
ir /2
0_
'-te
+
as F
.
:I/M
ar/2
014
Nitr
ate
as N
OB
-N
- -/
Mar
/20=
! Il
atft
e Il
-
f as
NO
2-N
S2£
<D
.1
02
ND
Kan
e
Dan
e
NO
-is
Nnt
s
iF_=
rcne
ar
ia
Ner
e
Xrs
e N
oce
Nar
a r
e
Le ,tr
e
NSr
e
tale
N
one
Nor
a
amt
CL
-GC
Ç 01
14
CC
GC
01
14
CC
GC
01
14
CC
GÇ
0114
_
-°C
011
4 _
- --
C
C
0115
-
-
11/M
ar/2
014
CC
GÇ
0115
11
/Mar
/201
4
esu1L
^_
Tot
a _,
_3c_
Har
dnes
s as
SM.-
ate.
-
-- '
5.8
30
897
118
99
1 PS
CC
GÇ
011
5 11
/Mar
/20.
14
-
CC
GC
_011
5 11
/M
--.
Nitr
ite e
s _-
_'
: C
CG
Ç01
15
11/
- PO
ta_o
. -
CCGC 01]5
CC
GÇ
0115
_.
.__1
1/M
a °
-/20
14
_ _ - -
C
CG
Ç 01
_-
_ r/
2014
_
_ _
C C
IEE
:_
r/20
14
- d
_sso
l ex
_'-
_ 1
. r/
2014
A
as
CaC
C=
C
CC
0116
11
/Mar
/20
14
Bi
ri ro
=
ce
- CCGÇ 01
16
..
11/Mar/2014
Cal
ti_.-
-_
_-
CC
GC
_011
6 11
/Mar
/201
4 C
hlo
_e
CC
GC
011
6 11
/Mar
/201
4 H
ardn
ess
as C
aC?3
C
CG
Ç 01
16
11/M
ar/2
014
Mag
nesm
m
CC
GÇ
0116
11
/Mar
/201
4 N
itrat
e +
Nitr
ite a
s '-:
CC
GÇ
0116
11
/Mar
/201
4 N
itrat
e as
NO
3-N
CC
G-_
0=1e
-
-_r/
20í4
:
-
:_. .
C
CG
D
E:_
_
r/20
14
_ ï =
-
5=16
11
/Mar
/201
4 So
dium
_.
.. -C
'16
11/M
ar/2
014
spen
fc-
'_:.-
, =
-__0
116
il/M
a "
4 su
lfat
e _
.._
CC
GÇ
0116
11
/Me-
CC
:' T
otal
Dis
solv
ed S
r- _
a C
OG
E 0
117
11/M
__
- A
lkal
inity
as
_
Cod
e `q
AC
bde
:
_ ..
317
_ 11
/Ma-
-C-'-
B
icar
bona
te
---0
0117
11
/Mer
-0t4
C
alci
um
=cr
em s
____
Z
GC
01
17
1/M
a..=
:_" }
Mag
nesi
um
11/M
ar -
,,Eat
N
itrat
e +
Nltr
rtea
s'-
-
1/M
a-S
ES
EA
N
itrat
e as
NO
3-N
11/M
a -=
]C=
N
itrite
as
NO
2-N
11/M
--
=C
4 Po
tass
es-
11/M
a. 1
'2_:
So
dium
11
/Ma-
i221
4 C
CG
C .
=1r
11
/Mar
a.15
51
Sulf
ate
CC
GÇ
"_
` 11
/Ma
-ZZ
C`
Tot
al D
iSer
.Ver
. -
"=
CC
GC
=
`18
11/M
ar/2
014
Alk
alin
ity a
s _`
03
CC
GÇ
0118
11
/Mar
/201
4 B
ice rb
- _e
ccer
_-
- - 11
/Maa
fEeD
a C
anitr
ids
- _
- 11
/Mar
-e2:
1-5
_
CC
GC
-:
11/M
ar-
_ M
a gne
sium
_
CC
GÇ
-5
11/M
,._=
Nitrat
= N
itrite
as`
: C
CG
C_0
118
11/M
a-12
:14
.._
.__
.. C
CG
Ç 01
18
CC
GÇ
311z
11
/Mar
ßL4
Pot
assi
u--'
121
700
328
400
161
173
scs
SS
55
CC
GC
_011
8 11
/Mar
1201
4 S
odiu
m
0000
12
8 D
J.
_ C
CG
C 0
118
11/M
ar/2
014
Spe
cific
Con
duct
ivity
15
51
0500
N
one
-000
0 00
05_-
C
CG
C
0118
11
/Mar
/201
4 S
ulfa
te
202
Non
e _.
_ C
CG
C_0
118
11 /M
ar /2
014
Tot
al D
isso
lved
Sol
ids
954
=
; N
one
CC
GC
_012
0 11
/Mar
/201
4 A
lkal
inity
as
CaC
O3
218
! _
Non
e -
- -
Mai
C
CG
C_0
120
11 /M
ar /2
014
Bic
arbo
nate
26
6 ',
=
Non
e
CC
GC
0120
11
/Mar
/201
4 C
alci
um
166
=
D
CC
GC
_012
0 11
/Mar
/201
4 C
hlor
ide
154
=
Non
e
CC
GC
0120
11
/Mar
/201
4 H
ardn
ess
as C
aCO
3 60
0 =
N
one
CC
GC
_012
0 11
/Mar
/201
4 M
agne
sium
45
=
D
CC
GC
_012
0 11
/Mar
/201
4 N
itrat
e-1-
Nitr
ite a
s N
3.
1 =
l
Non
e
CC
GC
_012
0 11
/Mar
/201
4 N
itrat
e as
NO
3 -N
3
=
I N
one
I
CC
GÇ
OIID
11
/Mar
/201
4 N
itrite
as
NO
2 -N
N
.1
¡ N
O
I N
one
CC
GC
_D12
0 11
/Mar
/201
4 P
otas
sium
5.
9 2 _
I D
__
_.
0505
050
0-
__ -0
0007
9 S
odiu
m
D
d
CC
GC
79
-0
-
_012
0 11
/Mar
7201
4 S
oi
_ D
0.
550_
- 5000
.. C
CG
C_0
120
11/M
ar/2
014
Spe
cific
Con
duct
ivity
13
30
!.
Non
e
CC
GC
_012
0 11
/Mar
/201
4 S
ulfa
te
221
=
I None
CC
GC
01
20
11 /M
ar /2
014
Tot
al D
isso
lved
Sol
ids
857
=
Non
e 04
5..
CC
GC
_012
1 12
/Mar
/220
14
Alk
alin
ity a
s C
aCO
3 14
4 N
one
CC
GC
01
21
12 /M
ar /2
014
Bic
arbo
nate
17
6 =
N
one
CC
GC
_012
1 _
12/M
ar/2
014
Cal
cium
15
7 _
! D
CC
GC
01
21
_
12/M
ar /2
014
Chl
orid
e !
143
1 =
N
one
CC
GC
01
21
12 /M
ar /2
014
Har
dnes
s as
C
532
I N
one
- 00
50
aCO
3 00
00__
=
__
C
CG
C_0
121
12 /M
ar /2
014 4
Mag
nesi
um
34
e D
CC
GC
_012
1 12
/Mar
/201
4 N
itrat
e +
Nitr
ite a
s N
47
.3
_ N
one
CC
GC
_012
1 12
/Mar
/201
4 N
itrat
e as
NO
3 -N
47
.2
=
l N
one
CC
GC
_012
1 12
/Mar
/201
4:
Nitr
ite a
s N
O2 -
N
0.1
i _
+N
one
CC
GC
_012
1 12
/Mar
/201
4 P
otas
sium
2.
5 =
D
CC
GC
0121
12
/Mar
/201
4 S
odiu
m
83
_ D
CC
GC
_012
1 12
/Mar
/201
4 S
peci
ficC
ondu
ctiv
ity
1365
=
N
one
CC
GC
_012
1 12
/Mar
/201
4 S
ulfa
te
103
=
I N
one
CC
GC
01
21
_ 12
/Mar
/201
4 i
Tot
al D
isso
lved
Sol
ids_
._
_928
' N
one_
C
CG
C 01
22
12 /M
ar /2
014
Alk
alin
ity a
s C
aCO
3 27
2 a
'Non
e C
CG
C_0
122
12/M
ar /2
014
Bic
arbo
nate
33
2 f
None
_._
0550
05
55 00
02 --
- 00
00 - 55
20
CC
GC
_012
2 12
/Mar
/201
4 C
alci
um
158
=
D
CC
GC
_012
2 12
/Mar
/201
4 C
hlor
ide
, 14
4 =
7
Non
e
CC
GC
_012
2 12
/Mar
/201
4 H
ardn
ess
as C
aCO
3 67
0 =
N
one
CC
GC
_012
2 12
/Mar
/201
4 M
agne
sium
67
-
D
CC
GC
_012
2 12
/Mar
/201
4 N
itrat
e +
Nitr
ite a
sN
24
=
Non
e
G
0012
_
..
r as
C
CG
C_0
122
12 /M
ar)2
014
Nitr
ate
as N
O3 -
N
23.9
=
N
one
CC
GC
_012
2 12
/Mar
/201
4 N
itrite
as
NO
2 -N
0.
1 _
Non
e
CC
GC
_012
2 12
/Mar
/201
4 P
otas
sium
4.
9 _
i
D
CC
GC
_012
2 12
/Mar
/201
4 S
odiu
m
136
=
D
CC
GC
_012
2 12
/Mar
/201
4 -'.
Spe
cific
Con
duct
ivity
17
23
=
Non
e
CC
GC
_012
2 12
/Mar
/201
4 S
ulfa
te
290
_ ,
Non
e
CC
GC
_012
2 12
/Mar
/201
4 T
otal
Dis
solv
ed S
olid
s 11
43
=
Non
e
CC
GC
_012
3 12
/Mar
/201
4 A
lkal
inity
as
CaC
O3
3]4
None
CG
C
0123
__
- C
CG
C01
23
12 /M
ar /2
014
Bic
arbo
nate
45
6 _
Non
e
CC
GC
01
23
12/M
ar /2
014
Cal
cium
23
8 -
! D
CC
GC
CC
GC
-023
...
._20
14
hloD
de _
0005
0550
_ 22
50 __
___0
123
12 /M
ar /2
014
Chl
orid
e 13
3 =
N
one
CC
GC
01
23
12/M
ar/2
014
Har
dnes
s as
CaC
O3
1101
=
i
Non
e
CC
GC
01
23
12 /M
ar /2
014
Mag
nesi
um
123
=
i D
CC
GC
01
23
12 /M
ar /2
014
Nitr
ate
+N
itrite
as
N
56.3
_
Non
e
CC
GC
01
23
12 /M
ar /2
014
Nitr
ate
as N
OS
-N
56.2
=
'. N
one
CC
GC
01
23
12 /M
ar /2
0142
N
itrite
as
NO
2 -N
0.
1 =
i
Non
e
CC
GC
01
23
12 /M
ar/2
014
Pot
assi
um
4.9
0 C
CG
C
0123
12
/Mar
/201
4 S
odiu
m
147
=
D
IP
IIé
r1Jf
R"s
1711
'áé
CC
GC
01
23
12 /M
ar /2
014
Spe
cific
Con
duct
ivity
22
81
=
Non
e C
CG
C 01
23
12 /M
ar /2
014
Sul
fate
45
2 =
N
one
CC
GC
01
23
' 12
/Mar
/201
4 T
otal
Dis
solv
ed S
olid
s 16
28
=
Non
e
CC
GÇ
0124
12
/Mar
/201
4 A
lkal
inity
as
CaC
O3
204
=
Non
e
CC
GC
01
24
12 /M
ar /2
014
Bic
arbo
nate
24
9 =
CC
GÇ
0124
12
/Mar
/201
4 C
alci
um
123
=
_'N
one
D
CC
GC
01
24
12 /M
ar /2
014
Chl
orid
e 91
=
N
one
CC
GC
_012
4 12
/Mar
/201
4 H
ardn
ess
as C
aCO
3 41
4 =
N
one
CC
GC
_012
4 12
/Mar
/201
4 M
agne
sium
26
=
D
CC
GC
_012
4 12
/Mar
/201
4 N
itrat
e +
Nitr
ite a
s N
26
-
=
Non
e
CC
GC
_012
4 12
/Mar
/201
4 N
itrat
e as
N
O3-
N
25.7
=
N
one
CC
GC
_012
4 12
/Mar
/201
4 N
itrite
as N
O2
-N
0.2
=
Non
e
CC
GC
01
24
12/M
ar /2
014
Pot
assi
um
1.8
=
:
D
CC
GC
01
24
12/M
ar/2
014
Sod
ium
71
=
D
{CG
C 0
124
12/M
ar/2
014
Spe
cific
Con
duct
ivity
10
68
e N
one
CC
GC
0124
12
/Mar
/201
4 S
ulfa
te
71
=
Non
e
CC
GC
01
24
12 /M
ar /2
014
Tot
al D
isso
lved
Sol
ids
657
i C
CG
C 01
25
12/M
ar/2
014
Alk
alin
ity a
s C
aCO
3 15
3 =
N
one
i C
CG
C 01
25
12 /M
at /2
014
Bic
arbo
nate
18
] _
Non
e
Í C
CG
C01
25
12 /M
ar /2
014
Cal
cium
12
3 =
D
CC
GC
01
25
12 /M
ar /2
014
Chl
orid
e 64
=
:
Non
e
CC
GC
0125
12
/Mar
/201
4 H
ardn
ess
as C
aCO
3 41
0 =
N
one
CC
GC
01
25
12/M
ar /2
014
Mag
nesi
um
25
=
D
_ _
CC
GC
01
25
_
12 /M
ar /2
014
Nitr
ate
+N
it r
te a
s i 4 403
=
Non
e
CC
GC
01
25
12 /M
a r/
2014
N
itrat
e as
NO
3 -N
40
_
Non
e C
CG
C
0125
12
/Mar
/201
4 as
NO
2 -N
03
=
N
one
I_. - -0
300_
C
CG
C_0
125
12/M
ar /2
014
Pot
assi
um
25
._. D
CC
GC
01
25
0125
. 2550
. C
CG
C
012.
5 12
/Mar
/201
4 S
odiu
m
00ti
2055
_
12/Mar/2014
Spe
cific
Con
duct
ivity
_
53
996
=
__
___
Non
e
CC
GC
0125
. 20
00. 12
/Mar
/201
4 S
ulfa
te
61
=
Non
e _o
.. 02
00_.
.
CC
GC
0125
12
/Mar
/201
4 T
otal
Dis
solv
ed S
olid
s 59
1 a
Non
e
CC
GÇ
0126
12
/Mar
/201
4 A
lkal
inity
as
CaC
O3
180
=
Non
e
CC
GC
0126
j
12 /M
ar /2
014
Bic
arbo
nate
20
=
N
one
LCC
GC
_012
6 12
/Mar
/201
4 C
alci
um
44
=
D
CC
GC
_012
fi 12
/Mar
/201
4 C
hlon
de
36
=
None
CCGC _0126
. -_-
:
2000
_ -_
12/Mar/2014
Har
dnes
s as CaCO3
155
155
_.
=
=
_ _
_ _
___
Non
e
If
CC
GC
01
26
12 /M
ar /2
014
Mag
nesi
um
.
11
- D
05
-01
5500
_..
CC
GC
01
26
2500
12JM
ar /2
014
N
.. as
N
itrat
e +
Nitr
ite a
s 0.
7 =
N
one
CC
GC
01
26
12/M
ar /2
014
Nitr
ate
as N
O3
-N
0.3
- N
one
____
_._.
._.
CC
GC
01
25
___
_..
____
._...
55
00. - 050
0..
_ _-
12
JMar
/201
4 N
itrite
as
NO
2 -N
..
0.4
_ _
_ =
__ _
_- - -_
,. N
one
CC
GC
01
26
12 /M
ar /2
014:
Po
tass
ium
2.
8 _
D
CC
GC
01
26
12 /M
ar /2
014
Sod
ium
53
_
D
CC
GC
01
26
12/M
ar /2
014
Spe
cific
Con
duct
ivity
49
6 e
Non
e
CC
GC
01
26
12/M
ar/2
014
Sul
fate
]
_ N
one
CC
GC
9126
12
/Mar
/201
4 T
otal
Dis
solv
ed S
olid
s 29
4 =
N
one
CC
GC
01
27
12 /M
ar /2
014
Alk
alin
ity a
s C
aCO
3 ,
193
=
Non
e
CC
GC
01
27
12 /M
ar /2
014
Bia
rbon
ate
235
5000
. -
=
Non
e
CC
GC
012
7 12
] 12
/Mar
/201
4 C
alci
um
/_
51
.._
_ D
CC
GC
01
27
12 /M
ar /2
014
Chl
orid
e 32
=
N
one
CC
GC
01
27
12/
12/M
ar/2
014
Har
dnes
s as
CaC
O3
189
=
Non
e
CC
GC
01
2]
CC
GC
_
0000
12
/Mar
/201
4 M
agne
sium
__
_
5000
_
CC
GC
0127
._
_ 12
/Mar
/201
4 N
itrat
e +
Nitr
ite a
s N
..
0.9
=
Non
e
CC
GC
01
2]
s 12
/Mar
/201
4 N
itrat
e as
NO
3 -N
0.
5 N
one
CC
GC
01
27
0052
12
/Mar
/201
4 N
itrite
as
NO
2 -N
.
0_..
0.4
0200
_._ =
Non
e
CC
GC
01
27
12 /M
ar /2
014
Pot
assi
um
2.6
=
CC
GC
01
27
12 /M
ar /2
014
Sod
ium
42
_
D
CC
GC
0127
12
/Mar
/201
4 ,
Spe
cìfic
CO
nduc
trvi
ry
503
_ N
one
el-3
5-ai
r.
Nam
e C
CG
C
0127
CC
GÇ
0127
CC
GC
0128
CC
GC
_012
8
CC
GC
_012
8 C
CG
C_0
128
CC
GC
01
28
CC
GC
01
28
CC
GC
0128
CC
GC
012
8 C
CG
C á
12ß-.
CC
GC
_012
8
CC
GC
_012
8 C
CG
CO
Y28
CC
GC
_012
8 C
CG
C01
28
CC
GC
_012
9 C
CG
C_0
129
CC
GC
0129
C
CG
C_0
129
CC
GC
_012
9 C
CG
C_0
129
_CCGC_0229-
CC
GC
01
29
CC
GC
_012
9 C
CG
C01
29
CC
GC
_012
9 C
CG
C_0
129
CC
GC
_o12
9
CC
GÇ
0129
C
CG
C_0
131
CC
GÇ
0131
C
CG
C_0
131
CC
GC
_013
1 C
CG
C01
31
CC
GC
_013
1
_
CC
GC
_013
1 C
CG
C
0- 1
31
CC
GÇ
0131
C
CG
C 0
131
CC
GC
_013
_
CC
GC
_01-
C
CG
C_0
___
CC
GC
_013
1 C
CG
C01
32
CC
GC
_013
2 C
CG
C_0
132
CC
GC
01
32
CC
GC
013
2 C
CG
C_0
132
CC
GC
01
32
CC
GC
0132
-
CC
GC
0132
C
CG
C_0
132
CC
GC
013'
CCGC_013`
CC
GC
013
2
12 /M
ä /2
014
Sum
_e
12/M
ar/2
014
s. - =_
_
12/Mar /2014
r
`
as C+
_ 12
/Mar
/201
4 =
s 12
/Mar
/201
4 !_
i-
12/M
ar/2
014
Chl
orid
e 'M
ar22
14
Har
dnes
s as
C 'C
3
,251
4-
e_
s.C
`N
_514
54
-4.5
4m
O14
.
^
12/M
ar/2
014
Sulf
ate
--
a/71
4 7c
tal
D!L
- ve
n So
lids
'_
-Im
tty a
sCaC
O3.
12
/51a
-r25
:14
trar
imna
te
12/M
ar02
014
_._ =-. _
- .. 12
/A9ä
/20i
4 _ _
502¡
14
Har
r±es
sasC
aCO
3 4.
-172
14
Mag
nesi
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__...
.
2514
N
itrat
e +
N.-
_ -_n
2 1/M
ar/2
014
Nitr
ate
as t-
4:
Mar
/201
4 N
it/ir
e as
N.3
2-h
12/M
er/2
014
50-2
s:4m
lia
-t5.
514
45.-
2454
n-
12/M
ar/2
014
Spec
ific
Cnn
duct
ivity
12
/Mar
/201
4 Su
lfat
e 12
/Mar
/201
4 T
otal
Dis
solv
ed Io
li_
13/M
ar/2
014
Alk
alin
ity a
s C
aCO
S _
13/M
ar/2
014
Bvc
arbo
-ete
15
/Mar
/201
4 C
alci
um
' 3/M
ar/2
014
l7do
rìde
_
_
/Mar
/231
,
-=_c
_.
3 -/
Mar
/27.
1e
_._.
, 13
/Mar
/201
4 N
itrat
e +
Ni_
-as
13/M
ar/2
014
Nitr
ate
as N
-h
13/M
ar/2
014
Nitr
ite a
sNC
2-t.
E._
13
/Mar
/201
4 Po
tass
ium
--
- 3.
2 -/
Mar
/201
4 So
_ï -
13/M
ar/2
014
Ss =
`._.
_c. .-
17
62
li/M
ar/2
014
S -.
_e
g-
+
-224
L
-
.c `_
13/M
ar/2
014
Bic
arbo
nate
_
13/M
ar/2
014
Cal
cium
13
/Mar
/201
4 C
hlor
ide
13/M
ar/2
014
Har
dnes
s as
CaC
O3
15/M
ar/2
5.14
M
agne
sium
-/
Mar
/20_
14
-+N
-eas
h /M
ar/2
C14
. tr
atea
st4 -
S
_4
V32
-7i
15./V
ar/2
014
23/M
ar/2
01-
SnoT
hrr
=
4-ne
=
F.^n
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Nic
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e
Kar
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ne
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05.4
54
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one
Kan
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CO
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01
33
CC
GC
C5.
55
CC
G
_
13 /M
ar /2
014
Tot
al D
isso
lved
Sol
ids
13/M
ar /2
014
Alk
alin
ity a
s C
aCO
3
33
Zar
/201
4 C
hlor
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r/20
14
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dnes
s -
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3
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s\
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NO
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15r/
2014
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lfat
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ar/2
014
Tot
al D
isso
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Sr
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lkal
n_
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13
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C-
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Pota
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13/M
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m
13/M
ar/2
014
Chl
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13/M
ar/2
014
Har
d - w
2 13
/Mar
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4 M
agne
sium
13
M
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14
Nita
ta+
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CC
5C 0
134
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CC
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CC
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CC
GC
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CC
GC
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CG
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13
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CG
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13/M
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314
Tot
al D
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CG
C
7135
14
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14
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14
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=
-s
s-_-
ç6
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014
____
03
96
----
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C03
96
- 20
14
_ fa
ts.
CC
039
6 `_
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tyas
CaC
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07/A
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07/A
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07
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7/A
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CC
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07/A
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07/A
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07/A
ug/2
014
Sulf
ate
-
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07/A
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07/A
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07/A
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07/A
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Z
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07/A
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014
Nitr
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+ N
itrite
=__
07./A
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2014
N
itrat
e as
NO
3-N
07/A
ug/2
014
Sodi
um
07/A
ug/2
014
Spec
ific
- __
-=-:
ty
07/A
ug/2
014
- z:
07
/Aug
/201
4 T
-_'-
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yed
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07/A
ug/2
014 ..
--
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07 /A
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07/A
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a_
07/A
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_ _-
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07/A
ug/2
014
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Fie
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eetti
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4-40
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r1
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8-
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07/A
ug/2
014
: N
itrat
e +
Nitr
ite a
s N
0.
2 =
N
one
07/A
ug/2
014
Nitr
ate
as N
O3-
N
<0.
1 N
D
Non
e
Nitr
ite a
s N
O2-
N
0.2
=
Non
e
Cr
4-_:
=11
:14-
P
otas
sium
2.
5
:
Non
e
27-
r_-_
-_T
-1-0
14
Sod
ium
18
5 =
=7
Z-4
ZZ
07
/Aug
/201
4 S
peci
ficC
ondu
ctiv
ity
1091
=
:-/4
_-_a
z-2:
14
Sul
fate
.
Noe
.
__
:7.
..g.-
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4 T
otal
Dis
solv
ed S
olid
s 58
5.-
=
.__
2814
A
lkal
iniry
as
CaC
O3
=5
- N
one
:CG
: :4
81
07/A
ug/2
014
Bic
arbo
nate
24
: -
Non
e
CC
G":
.7
,4-2
1 07
/Aug
/201
4 C
alci
um
55
=
'r- D
07/A
ug/.7
.71:
.7
-_or
ide
114
=
Non
e
07/A
ug/Z
1.:
-a-d
ness
as
CaC
O3
203
,
=
Non
e
ZC
GC
:-
Ci
07/A
ug/2
014
Vag
nesi
um
=
___i
D
1CG
C_0
4:1
07/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
0.9
=
Non
e
C-C
GC
O
C
1C-A
ug/2
014
Nitr
ate
as N
O3-
N
06
Non
e
ZC
GC
O
C
21-A
ug/2
014
Nitr
ite a
s N
O2-
N
0.2
, =
i
Non
e
GC
_04:
: :-
-Aug
/201
4 P
otas
sium
D
C:5
: :-
----
:1
77 -A
ug/2
014
Sod
ium
:
98 - =
,
:CG
: :2
.:1
:- A
ug/2
014
,..
Spe
cific
Con
duct
ivity
79
8 =
I
Non
e
:CG
C C
IL::
07/A
ug/2
014
Sul
fate
'
26
=
Non
e
ZC
GC
04
:: 07
/Aug
/201
4 T
otal
Dis
solv
ed S
olid
s -
482
=
Non
e :C
GC
:4:
: 07
/Aug
/201
4 A
lkal
inity
as
CaC
O3
. 99
=
N
o-e
ZZ
EC
f/:
1_
07/A
ug/2
014
Bic
arbo
nate
'
121
=
No-
:e
1-C
2C 04
:i 07
/Aug
/201
4 _
Cal
cium
_ 1
'
- D
ZZ
GC
O
C
07/A
ug/2
014
, C
hlor
ide
- - =
N
one
ZC
GC
1r
:2
0- -A
ug/2
014
Har
dnes
s as
CaC
O3
4-25
=
N
one
:7 A
ug/2
014
: M
agne
sium
38
h
:Z5Z
_Z-f
:: 7T
/Aug
/201
4 N
itrat
e +
Nitr
ite a
s N
56
.1
Non
e Z
=C
04:
: 07
/Aug
/201
4 N
itrat
e as
NO
3-N
56
=
N
one
:CG
C 04
:1
07/A
ug/2
014
Nitr
ite a
s N
O2-
N
: 0.
2 -
Non
e
7.18
C 0
4::
07/A
ug/2
014
Pot
assi
um
- - D
.1:8
C 0
4:.:
07/A
ug/2
014
Sod
ium
61
.=
F
D
ZC
GC
04
:: 07
/Aug
/201
4 S
peci
ficC
ondu
ctiv
ity
j 11
22
- i
Non
e _
:C _o
4::
07/A
ug/2
014
Sul
fate
65
=
N
one
2:20
_04:
: 07
-Aug
/201
4 T
otal
Dis
solv
ed S
olid
s ,
815
- :
Non
e
:15C
;ln
Z7A
ug/2
014
Alk
alin
ity a
s C
aCO
3 15
5 =
N
one
Z.7
-GZ
:-
4:3
:-'
Aug
/201
4 B
icar
bona
te
89
=
i
Non
e
C.:3
C o
c-
:7 'A
ug/2
014
Cal
cium
189
D
-.1-
0GC
:::
- :7
-Aug
/201
4 C
hlor
ide
. 96
=
-
Non
e ,
CS
C :
r.-:
5 17
_ A
ug/2
014
Har
dnes
s as
CaC
O3
. 31
5 .
=
Non
e
ZC
GC
:-
C3
07/A
ug/2
014
Mag
nesi
um
28
;
=
D
:CG
C 04
:8
77_
Aug
/201
4 ;
Nitr
ate
+ N
itrite
as
N
22.4
=
N
:C/A
ug/2
014
Nitr
ate
as N
O3-
N
22.2
=
N
one e
ZT
/Aug
/201
4 '
Nitr
ite a
s N
O2-
N
0.2
=
__1
Non
e
2--G
C 0
4-5
07/A
ug/2
014
Pot
assi
um
D
=G
CZ
-4Z
E.
07/A
ug/2
014
Sod
ium
.
59
=
i D
7CG
C11
4:5
07/A
ug/2
014
Spe
cific
Con
duct
ivity
88
5 ,
=
Non
e
:CG
C
7-:.7
.5
07/A
ug/2
014
Sul
fate
58
=
N
one
:CG
C 0
4:5
07/A
ug/2
014
Tot
al D
isso
lved
Sol
ids
542
=
Non
e
:050
040
4 07
/Aug
/2-0
14
Alk
alin
ity a
s C
aCO
3 14
5 .
=
Non
e
:CG
C
0404
07
/Aug
/201
4 B
icar
ate
, 17
7 =
N
one
Z:2
0_04
04
07/A
ug/2
014
Ca
r.-_
,-
, 15
8 =
D
:CG
C
0404
07
/Aug
/201
4 C
l, 5-
-da
269
=
Non
e
07/A
ug/2
014
Har
dnes
s as
CaC
O3
609
=
No-
e
07/A
ug/2
014
Mag
nesi
um
52
: =
D
CC
GC
_04:
2.
07/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
38.9
=
N
r-_,
mat
ingi
alip
pa
.4.tr
4iat
n.w
ent,l
z.op
soa
v.5,
v;14
07
,AN
SOPI
SIO
W,,g
4.
:440
40S0
WW
:-M
.,Tig
t -'4
03es
Utt1
'3.-
'
4Clf
idft
te<
Non
e C
CG
C
0404
38
.7
-07/
Aug
/201
4
Nitr
ate
as N
OS
-N
CC
GC
04
04
07/A
ug/2
014
_ N
itrite
as
NO
2-N
0.
2 =
N
one
CC
GC
04
04
07/A
ug/2
014
Pot
assi
um
3:
- _
CC
GC
04
04
07/A
ug/2
014
Sod
ium
F
E
- C
CG
C 04
04
07/A
ug/2
014
Spe
cific
Con
duct
ivir;
-_
=
CC
GC
04
04
07/A
ug/2
014
Sul
fate
64
=
...
_ _
CC
GC
04
04
07/A
ug/2
014
Tot
al D
isso
lved
Sol
ids
_ .
_
Non
e
CC
GC
04
05
07/A
ug/2
014
Alk
alin
ity a
s C
aCO
3 -
CC
GC
04
05
07/A
ug/2
014
Bic
arbo
nate
-
. _-
- =
ce
-
CC
GC
04
05
07/A
ug/2
014
Cal
cium
89
-
CC
GC
13
405
07/A
ug/2
014
Chl
orid
e =
CC
GC
040
5 07
/Aug
/201
4 H
ardn
ess
as CaCO3
,' 39
393
,
- C
CG
C_0
405
07/A
ug/2
014
Mag
nesi
um
27
- C
CG
C 04
05
07/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
3.6
- C
CG
C 04
05
07/A
ug/2
014
Nitr
ate
as N
OS
-N
3_5
- N
one
CC
GC
04
05
07/A
ug/2
014
Nitr
ite a
s N
O2-
N
- -
=
___
CC
GC
04
05
07/A
ug/2
014
Pot
assi
um
,
3:
=
CC
GC
040
5 --
_
: C
CG
C 04
05
07/A
ug/2
014
Sod
ium
07/A
ug/2
014
Spe
cific
Con
duct
ivity
83
8 =
CC
GC
040
5 07
/Aug
/201
4 S
ulfa
te
67
- 00
80 _0
405
07/A
ug/2
014
Tot
al D
isso
lved
Sol
ids
510
. -
Non
e C
CG
C
0406
07
/Aug
/201
4 A
lkal
inity
as
CaC
O3
- - N
one
CC
GC
04
06
, 07
/Aug
/201
4 B
icar
bona
te
=
Non
e
CC
GC
04
06
07/A
ug/2
014
Cal
cium
-
D
CC
GC
04
06
'
11;4
._
-5
=
07
/Aug
/201
4 C
hlor
ide
CC
GC
04
06
299
- c-
e 07
/Aug
/201
4 H
ardn
ess
as Z
att-
5-
- -
CC
GC
04
06
07/A
ug/2
014
Mag
nesi
_ =
-
- ,
24
- r-
- C
CG
C 04
06
- 07/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
_ C
CG
C
0406
07
/Aug
/201
4 N
itrat
e as
N
O3-
N
_ _
=
CC
GC
04
06
07/A
ug/2
014
Nitr
ite a
s '1
/202
0.
3 .._
-
07/A
ug/2
014
Pot
assi
u-
3.6
- C
CG
C
0406
D
Non
e
CC
GC
04
06
07/A
ug/2
014
Sod
ium
__
=
-1
- C
CG
C
0406
07
/Aug
/201
4 S
peci
ficC
ondu
ctiv
ity
- I
Non
e
CC
GC
04
06
07/A
ug/2
014
Sul
fate
1E
- -
CC
GC
04
06
_ 07
/Aug
/201
4 T
otal
Dis
solv
ed S
olid
s ,..
_..-
-
CC
GC
04
30
08/A
ug/2
014
Alk
alin
ity a
s C
aCO
3 _ _,
=
CC
GC
_043
0 '
08/A
ug/2
014
Bic
arbo
nate
15
1 =
N
one
U.G
C
0430
08
/Aug
/201
4 C
alci
um
62
=
CC
GC
04
30
, N
one
CC
GC
04
30
08/A
u8/2
014
Chl
orid
e
08/A
ug/2
014
Har
dnes
s as
C
aCO
3 --
, =
08/A
ug/2
014
Mag
nesi
um
=
CC
GC
04
30
0Non
e
08/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
- - N
one
LI
cCce
CG
cC
0404
3300
08
/AU
g/20
14
Nitr
ate
as N
O3-
N
1:.7
=
N
one
LCC
GC
04
30
0.2
- 08
/Aug
/201
4 N
itrite
as
NO
2-N
' 08
/Aug
/201
4 P
otas
sium
2.
6 =
C
CC
C_0
430
Non
e
CC
CC
_043
0 15
'
_ 06
/Aug
/201
4 S
odiu
m
CC
GC
04
30
493
=
08/A
ug/2
014
Spe
cific
Con
duct
ivity
08/A
ug/2
014
Sul
fate
67
e
Non
e e
CC
GC
04
30
CC
GC
04
30
Non
e 08
/Aug
/201
4 T
otal
Dis
solv
ed S
olid
s 30
8 =
_
CC
Gm
ai
08/A
ug/2
014
Alk
alin
ity a
s C
aCO
3 21
4 =
C
CC
GC
04
31
08/A
ug/2
014
Bic
arbo
nate
26
1 -
=
: N
one
CC
GC
04
31
08/A
ug/2
014
Cal
cium
-
. -
CC
GC
04
31
08/A
ug/2
014
Chl
orid
e 87
=
CC
GC
04
31
08/A
ug/2
014
Har
dnes
s as
C
aCO
3 1.
:.:
=
Non
e
CC
GC
04
31
'
08/A
ug/2
014
Mag
nesi
um
37
- =
D
ccG
c 04
31
33.6
-
=
',Non
e 08
/Aug
/201
4 N
itrat
e -s
N
itrite
as
N
CC
GC
04
31
08/A
ug/2
014
Nitr
ate
as N
O3-
N
Non
e _
m
Sam
pld0
a*
ìnáy
reN
ame
`l dë
CC
GC
_043
1 CCGC 0431
CC
GC
0431
C
CG
C 0
431
CC
GC
_043
1 C
CG
Ç 04
34
CC
GC
_043
2 C
CG
C_°
^2
CC
GC
-4
2 C
CG
C
0432
C
CG
C
0432
CC
GC
0432
CC
GC
0432
C
CG
C 0
432
CC
GC
0432
C
CG
C04
32
CC
GC
0432
C
CG
C_0
432
CC
GC
_043
2 C
CG
C04
32
CC
GC
0433
C
CG
C_0
433
CC
GC
_043
3
CC
GC
_w -
CC
GC
14
33
CC
GC
'422
C
CG
C C
zE3
CC
GC
C
a5S
CC
GC
_043
3 C
CG
C
0433
CfS
aC 04
33
CC
GC
_043
3
-CC
GC
_044
1 C
CG
C
0441
C
CG
C
0441
C
CG
C 0
442
CC
GC
044
1
CC
GC
_044
1
CC
GC
_044
1 C
CG
C_0
441
CC
GC
04
41
CC
GC
_044
1 C
CG
C
0441
CC
GC
0441
CC
GC
_044
1 C
CG
C 0
441
CC
GC
_044
2 C
CG
C
0942
:CSC
C-1
12
CC
GC
C
-=
CC
GC
==
--2
CC
GC
'-4I2
C
CG
C "'
-
1261
4 N
itrite
as
Ntt2
- @
1112
14
Pota
ssiu
m
2014
:
08/A
ug/2
014
: _--
3r;it
e 06
/Aug
/201
4 S4
fate
08
/Aug
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Har
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08/A
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08
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14/A
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14/A
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14/A
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14/A
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14/A
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14/A
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14/A
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014
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14/A
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014
Har
dnes
s _
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., -f
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044
4- -
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Aug
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4 H
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at tt
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21
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503
503
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73
334
226
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14 /A
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014
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4 1=
Aug
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2014
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N
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14 /A
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Aug
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1 :r
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14 /A
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14 /A
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____
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443
ug/2
014
Sp
°cC
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443
1- =
ug/
2014
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Sul
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69
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Sul
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69
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4 T
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solv
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30
6
= =
ug/
2044
T
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s 30
6
25 .L
ug /2
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Alk
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ity a
s C
aCO
3 13
7
13.=
ug/
2014
B
icar
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te
- 16
7
27/A
ug/2
014
Cal
cium
16
1
27/A
ug/2
014
Chl
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0
27/A
ug/2
014
Har
dnes
s as
CaC
D3
567
_ -
27/A
Ug/
2014
M
agne
sium
40
27 /A
ug /2
014
Nitr
ate
+ N
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as
N
5_=
27
/Aug
/201
4 N
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N
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56
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__
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NO
2 N
0.
3
-
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_
ssium
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__
___
__
= 7
lrug/
2014
S
peci
ficC
ondu
ctiv
ity
1359
r..p
ug/2
014
Sul
fate
10
5
_ =
ug/
2014
I
Tot
al D
isso
lved
Sol
ids
983
- --
eug/
2014
A
lkal
inity
as
CaC
O3
161
:= -
=ug
/201
4 B
icar
bona
te
196
27/A
ug/2
014
Cal
cium
67
27/A
Ug/
2014
C
hlor
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174
27/A
ug/2
014
Har
dnes
s as
CaC
O3
291
27/A
ug/2
014
I M
agne
sium
30
SF
/Aug
/201
4 '
Nitr
ate
+N
itrite
as
113
-/H
VQ
/LU
14
Nm
atea
27/A
ug/2
014
Nitr
ite a
s N
O2-
N
0.3_
_ 27
/Aug
/201
4 P
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sium
2
27 /A
ug/2
0"
Ebb
s _m
95
27 /A
ug/2
0::
- = _f
ccon
duct
ivity
10
15
27/A
ug/2
0::
S.
fate
34
27/A
ug/2
014
Tot
al D
isso
lved
Sol
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-
600
27/A
ug/2
014
Alk
alin
ity a
s C
aCO
3 20
6
27/A
ug/2
014
Bic
arbo
nate
25
1
27/A
ug/2
014
Cal
cium
94
27/A
ug/2
014
Chl
orid
e 10
5
27 /A
ug/2
014
Har
dnes
s as
CaC
O3
399
27 /A
ug/Z
C
:`ag
nesi
um
40
.__
27/A
Ug/
20}
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NSr
re.
as _
- 16
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27 /A
ug /2
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16.3
27/A
Ug/
201'
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as
NO
2 -N
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4 27
/Aug
/201
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cass
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3.
8
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=
D
=
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e =
N
one
=
Non
e =
N
one
=
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e N
one
=
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=
D
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one
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one
=
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Non
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one
=
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N
one
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=
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N
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e N
one_
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one
=
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=
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one
=
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=
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e
=
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one
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one
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one
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one
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one
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one
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one
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27_-
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Str
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S_
.
J3
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047
4 27
/AU
g/20
14
Spe
cific
oond
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iry
1133
e
Non
e
CC
GC
04
74
27/A
ug/2
014
Sul
fate
15
6 =
=
Non
e
Non
e C
CG
C04
74
CC
GC
_047
5
27/A
ug/2
014
28 /A
ug/2
014
Tot
al D
isso
lved
SO
-_
tutu
-
Alk
alin
ity a
s C
aCO
3
703
315
_._.
. =
N
one
CC
GC
04
75 _ -
-_
CC
GC
. 047
5 C
CG
C_0
475
28 /A
ug/
28 /A
U
- 28
/Aug
_
tic r
bona
te
_ da
rn
384
tutu
tut
u 125
=
_._
_ N
one _
D
-- o
ride
FE
-_
=
= e =
Non
e N
one
CC
GC
04
75
28 /A
ug/2
014
Har
dnes
s as
CaC
O3
CC
GC
04
75
CC
GC
04
75
28/A
ug/2
014
28/A
ug/2
014
Mag
nesi
um
Nitr
ate
Nitr
ite a
s N
s-
__
0.7
D
Non
e C
CG
C
0475
28
/Aug
/201
4 i
Nitr
ate
as N
O3
-N
0.3
=
Non
e
CC
GC
04
75
28/A
ug/2
014
r N
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as
NO
2 -N
0.
4 -
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e
D
CC
GC
04
75
28/A
ug/2
014
Pot
assi
um
4.8
=
CC
GC
04
75
_.._
tut
u _ -
CC
GC
04
75
-
CC
GC
04
75
CC
GC
04
75
28 /A
ug/2
014
-_-
28/A
Ug/
2014
28
/Aug
/201
4
Sod
ium
S
peci
ficC
ondu
ctiv
ity
__
___
_ -
- _.
_..
:Fr
_ _ e
'cm
_ 28
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/201
4 =
s= v
ed S
olid
s C
?_
86
_ 203
s me
CC
GC
04
76
28 /A
ug /2
014
A
- as
CaC
O3
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C
CG
Ç 04
]6
28 /A
ug /2
014
Bic
arbo
nate
CC
GC
0476
28/Aug/2014
Calcium
122
_
= Non
e C
CG
C_0
476
28/A
ue/2
014
28/A
ug/2
014
Chl
orid
e 12
6
CC
GC
0476
'
Har
dnes
s as
CaC
O3
552
= e =
Non
e C
CG
C 04
76
28/A
ug/2
014
28/A
Ug/
2014
M
agne
sium
N
itrat
e +
Nitr
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s '4
60
139
O
Non
e C
CG
C 04
76
CC
GC
04
76
28/A
ug/2
014
Nitr
ate
as
NO
3 -N
14
1 _
D
CC
GC
04
76
28 /A
ug/2
014
Nitr
ite a
s N
O2-
N
Pot
assi
um
.__
Sod
ium
_t
utu_
_ -
Spe
cific
Con
duct
ivity
_.
_
03
4 - -
31J
127
e =
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e __
_ p
___t
utu-
C
CG
C 04
76
CC
GC
04
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CC
GÇ
04]6
_ ._
_ 28
/Aug
/201
4 28
/A
ß/2
O14
28 /A
Ug/
2010
. =
_ i
=
Ycne
`.cr
ie
\one
C
CG
C
0476
-
28/A
ug/2
014
- S
ulfa
te
CC
GC
04
76
28/A
ug/2
014
Tot
al D
isso
lved
Sol
ids
1371
CC
GC
_047
7
CC
GC
_047
7
28 /A
Ug/
2014
28/A
ug/2
014
Alk
alin
ity a
s C
aCO
3
Alk
alin
ity a
s C
aCO
3 ut
u__ 16
3 -
tutu
___-
r.
-ne
_ _
CC
GC
_047
7
CC
GC
_047
7 ! -
_ C
CG
C 04
77
28 /A
ug/2
014
Alk
alin
ity a
s C
aCO
3 16
3 - e
+cn
e
28/A
ug/2
014
- .._
...
28/A
Ug/
2014
B
icar
bona
te
Bic
arbo
nate
=
Non
e
--=
=
_
Non
e N
one
CC
GC
_047
7 28
/AU
g/20
14
1 B
icar
bona
te
199
CC
GC
_047
7 28
/Aug
/201
4 C
alci
um
52
52
- _
D
CC
GC
04
77
28 /A
ug _
_ C
alci
um
-
e =
=
ID
D
_ N
one
Non
e
CC
GC
04
77
CC
GC
04
A
CC
GC
_047
7 ,.
28 /A
U_
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28
/A
1 ..
_.__
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28/A
Ug/
2014
Cal
cium
Chl
orid
e -.
.. C
hlor
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52
tutu
AO
340
ujsc
_047
7 28
/Aug
/201
4 C
hlor
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340
_ N
one
.cne
C
CG
C_0
477
CC
GÇ
0477
28 /A
ug /2
014
28 /A
ug /2
014
Har
dnes
s as
CaC
O3
Har
dnes
s sC
aCO
3
274
274
_ __
_.._
..
CC
GC
04
77
CC
GC
047
7 -
28 /A
ug/2
014
Har
dnes
s as
CaC
O3
274
_ N
one
28/A
ug/2
014
28/A
ug/2
014
Mag
nesi
um
35
35
_ e
_ D
_
-'!
CC
GC
_047
7 M
agne
sium
C
CG
C
0477
28
/Aug
/201
4 28
/Aug
/201
4 ,
Mag
nesi
um
I N
itrat
e +
Nitr
ite a
s N
35
5.8
_ _
_ . =ne
C
CG
C_0
477
CC
GC
_047
7 28
/Aug
/201
4 I
Nitr
ate
+ N
itrite
as
N
5.8
CC
GÇ
0477
23
/Aug
/201
4 N
itrat
e +
Nitr
ite a
s N
5.
8
_
CC
GC
_047
7 28
/Aug
/201
4 N
itrat
e as
N
O3
-N
=.E
CC
GC
_047
7 28
/Aug
/201
4 N
itrat
e as
N
O3
-N
¡ E
s:
Non
e C
CG
C_0
477
28/A
ug/2
014
Nitr
ate.
as
NO
3 -N
j
5.6
CC
GC
_047
] 28
/AU
g/20
14
Nitr
ite a
s N
O2
-N
02
=
Non
e
000C
04
77
28 /A
ug /2
014
Nitr
ite a
s N
O2
-N
02
_ '..
rne
Fie
ld -o
ir N
E-n
e S
e+ip
4eL
ie .
: A
nal
C
CC
GC
04
77
CC
GC
04
77
ccG
C_0
477
CC
GÇ
047
7
CC
GC
_r ï
CC
GC
_z-
CC
GC
04
- 77
CC
GC
04
77
cCG
C
0477
ccG
C_0
47)
CC
GC
_047
7
CC
GC
_047
7
CC
GC
_047
7
CC
GC
_047
7
CC
GC
_047
7
CC
GC
0483
CC
GC
_048
3
CC
GÇ
0483
cCG
Ç 04
83
CC
GC
_048
3 C
CG
C 0
483
GÇ
0483
CC
GC
_048
3
CC
GC
04
83
CC
GC
_048
3
CC
GÇ
0483
CC
GC
_048
3
CC
GC
_048
3
CC
GÇ
048
3
CC
GC
_048
4
CC
GC
_048
4
CC
GC
04
84
CC
GC
048
4
CC
GC
_048
4
CC
GC
_048
4
CC
GC
_098
4
CC
GC
04
84
CC
GC
_048
4
CC
GC
_048
4
CC
GG
048
4
CC
GC
_048
4
_CC
GC
_048
4 Lt
bC_0
484
CC
GÇ
0487
CC
GC
_048
7
CC
GC
_048
7
CC
GC
0487
CC
GC
_048
7
CC
GC
_048
7
CC
GÇ
0487
C
CG
G
048.
7
CC
GC
04
87
CC
GC
_048
7
C4.0487
CCGC2687-.
CC
GC
04
87
2014
28/A
ug/2
014
28/A
ug/2
014
28/A
ug/2
014
28/A
72
014
28/A
4z71
314
28/A
'.'
_ 28
/Aug
/201
4 28
/Aug
/201
4
Writ
e as
NO
2 -N
P
otas
sium
tsss
n--
-item
Sat
28
/Aug
/201
4 s
ccG
na-
.
28/A
ug/2
014
28/A
ug/2
014
5.44
azs
28/A
ug/2
014
Sul
fate
28
/Aug
/201
4 T
otal
Dis
solv
ed S
olin
s
28/A
ug/2
- 28
/Aug
/2C
1 sc
t
eed
Sol
ids
27 /A
ug/2
014
27/A
ug/2
014
B-
' -. _ _
27
/Aug
/201
4 Q
kfum
`
_..
27/A
ug/2
014
Chl
orid
e
27/A
ug/2
014
Har
dnes
s as
tace
t 27
/Aug
/201
4 M
agne
sio-
27
/Aug
/201
4 N
itrat
e F
._ t
e _
N
27 /A
U 41
4 -
27 /A
ug/2
:7,_
4
27/A
ug/2
014
Pot
assi
um
27/A
ug/2
014
Sod
ium
27
/Aug
/201
4 cp
ificconc_
27/A
ug/2
014
Sul
fate
27
/Aug
/201
4 T
otal
Dis
se a
ra±
Soh
o-a
27 /A
ug/2
014
Alk
alin
ity a
scac
s 27
/Aug
/201
4 B
icar
bona
te
i_
014
C
27 /A
ug/2
014
Har
dnes
s as
:a
CC
I 27
/Aug
/201
4 M
agne
sium
27
/Aug
/201
4 N
itrat
e +
N;-
t.4_
as'=
27
/Aug
/201
4 N
itrat
e as
NO
S -N
27/A
ug/2
014
Nitr
ite a
s N
52-1
27
/Aug
/201
4 P
otas
sium
27/A
ug/2
014
Sod
ium
27
/Aug
/201
4 S
P
-==
c= _
-bt
r 27
/Aug
/201
4 S
u =
e 27
/Aug
/201
4 T
otal
Dis
so'=
-Sas
26
/Aug
/201
4 A
lkal
inity
as
:aC
C=
26/A
ug/2
014
Bic
arbo
nate
26/A
ug/2
014
Cal
cium
26/A
ug/2
014
Chl
orid
e
26/A
ug/2
014
Har
dnes
s as
CaC
__
26/A
ug/2
014
Mag
nesi
um
c kf
tr.te
-74
rite
as _
2 _tete
28/A
ug/2
014
Nitr
:te a
s N
it : °-
_ _4
264A
ug/2
014
25/A
ug/2
014
Saz
-
- _c
u.z
d r 1A
ug/2
014
Sul
_Y
374
kons
C_e
Non
e N
rie
tre
Non
e
Nor
a
acne
t-e
Nor
e N
one
Non
e
tre
R^e
4_-e
N
one
51
=
D
n-_
_ N
o-t
Non
e
Flaldpoint
Námë
QA
Cod
è ..:
CC
GC
_048
7
CC
GÇ
0488
CO
G-
C4E
_
C G
C
-__
CC
G'
^4E
c
CC
G_ s=
C
CG
__- -
CC
GC
_=L
S-V
e
CC
G_ .t-
_4
88
CC
GC
_048
8
CC
GÇ
0488
CC
GC
_048
8
CC
GC
_048
8
CC
GC
_
CC
GÇ
CiE
2
CC
GÇ
C48
3 27
/Aug
/201
4 C
CG
C 0
4E9
27/A
ug/2
014
CC
GC
248
9 27
/AU
g/20
14
CC
GC
C
4Es
27/A
ug/2
014
CC
GC
_+
? -
_ 20
14
CG
C 4
:4-4
74
LT-4
.,e '2
014
27/-
Aug
/201
4
27/A
ug/2
014
27/A
uge-
23:4
C
CG
C
4,46
0 27
/Aug
/C:::
C
CG
C 0
49.3
27
/Aug
.-=
1.=
-
27/A
ug/2
014
'
27/A
ug/2
014
CC
GC
04
90
__--
-
_ -
_
CC
GC
049
0 -'
.'049
0-..
- -
CC
GÇ
0490
...
27
-u
CC
GÇ
049
0 27
/AU
,2_
_ C
CG
C
0490
27
/Aug
--2.
7:4
CC
GC
.049
0 27
/Aug
/201
4 C
CG
Ç 04
90
27/A
,=
7201
4
27/A
t "C
` =
27/A
ugre
fla
CC
GC
049
_
_1-
CC
GC
C
491
_-
CC
GG
_=
°_
277.
44'4
;201
4 C
CG
C
-91
27/A
ug.,.
-201
4_
CC
GC
-_
C
CG
C
'
27/A
ug.-
24i4
C
CG
C i5
1 27
/A:4
, 22 _
CC
GC
Cet
--
CG
C 0
431
CC
GÇ
049
1
CC
GC
_049
1 _a
_'=
91
uß/2
014
Tot
al D
isso
lved
Solids
Alk
alin
ity a
s C
aCO
3
Bic
arbo
nate
...
C
aldu
- C
hlor
t -e
Har
d _s
s as
_`
73
177A
....g
/201
4 ß
/201
4 =
cm_
27/A
ug/2
014
- 27
/Aug
/201
4 _
_
- _c
- ..
27/A
-4-2
,1: -4
' 27
/Aus
7=4
Tot
al D
isso
lver
So is
27
/Au
_C
a A
lkal
inity
as
- -_
_s
27 /A
ua _
_4
Bic
arbo
nate
27/A
7-=
=
Cal
cium
--
-- H
e-fr
ee-a
as
Sa 20
3
a 44
1>\
Nitr
ite a
s N
O2-
rJ
Pot
assi
um
Sod
ium
-
Spe
cìflc
cCon
duct
ivi-.
54
za:
e
Alk
alin
ity a
s C
aCC
E
Bic
arbo
nate
C
alci
um
Chl
orid
e H
ardn
ess
as a
ce
Mag
nesi
um
Nitr
ate
+ N
itrite
as
N
Pot
assi
um
Sod
ium
Spe
cd¢C
ondu
ctiv
i-;,
Sul
fate
T
otal
Dis
solv
ed S
o!S
A
lkal
inity
as
CaC
O3
Bic
arbo
nate
Har
dnes
s as
Cac
a M
agne
sium
N
itrat
e +
Nitr
ite a
=_"
:
Nitr
ate
as N
O3
-N
__- ï a1
=
Sc_
z r
27/A
ug)2
014
Spe
cdic
C n
duct
ivi .-
_.
...
27/A
Ug/
2014
S
ulfa
te
27/A
ug/2
014.
T
otal
D
546
339
414
82
78
394
46
4.2
os
2.6 15
680
171
209
258
424
1081
104
2444
Non
e
Non
e
Non
e
Non
e
Non
e D
Non
e N
one
Non
e
Non
e D
Non
e N
one
Non
e
Non
e
D
Non
e
145
Non
e
r F
ëldP
nínt
m
27/A
ug/2
014
.
Alk
alin
ity a
s C
aCO
3 24
7
27 /A
ug/2
014
Bic
arbo
nate
30
1
27/A
ug/2
014
Cal
cium
13
9
27/A
ug/2
614
Chl
orid
e 11
1
:CG
C
04E
, 27
/Aug
/201
4 H
ardn
ess
as C
aCO
3
:CG
C
0432
27
/Aug
/201
4 M
agne
sium
=w
C_0
432
27/A
ug/2
014
Nitr
ate
+ N
itrite
as
N
_SG
C_0
4E-
27/A
ug/2
014
Nitr
ate
as N
O3-
N
: 21
.4
.
:CG
C
0431
27
/Aug
/201
4 N
itrite
as
NO
2 -N
CCGC
_
27/A
ug/2
014
Pot
assi
um
3.8
Cc
=_
= -S
27
/Aug
/201
4 S
odiu
m
i 12
2 =
D
:CG
C_0
492
-7/A
ug/2
014
Spe
cific
Con
duct
ivity
15
60
=
Non
e
SG
C_0
492
r7/A
ug/2
014
Sul
fate
34
8 =
N
one
ZC
GÇ
04"_
IT
/Aug
/2:::
l D
isso
lved
Sol
ids
1083
e
Non
e -_
- _
- -
- .._
_.._
.__.
__
_ C
GC
04=
_
- /A
Ug/
Z-
_ lìn
ity a
s C
aCO
3 29
4 _
: N
one
LCG
C 0
493
:7 A
ug /_
__'
e ts
rbon
ate
¡ 35
9 -
_ e
_ - -__
- -.
. =
CC
043
5 /A
ug/_
-
-_m
28
1 -
_
:CG
C _
04=
2 7_
-A
_ 7
z _-
-ond
e 23
5 _
c __
C
CG
C
__
Har
dnes
s as
- =
"=
1340
=
N
one
Mag
nesi
um
155
D
/Aug
/201
4 N
itrat
e tr
ate
+ N
itrite
as
N
116
=
Non
e _-
--
-.
Aug
/201
4 N
i trat
e as
N
O3 -
N
117
- -D
:CG
C
0493
_
/Aug
/201
4 N
itrite
as
NO
2 -N
0.
4 -
- N
one
siu
:CG
C _
0493
27
/AU
g/20
14
Pot
assi
um
4.7
l -
D
CG
C_0
493
27/A
ug/2
014
Sod
ium
l
215
D
L N
one
' N
one
D
Non
e
Non
e
D
Non
e N
one
_ N
one.
..___
___.
D
CC
GC
04
93
27/A
ug/2
014
Spe
cific
Can
duct
ivity
30
32
=
No-
e
CC
GC
_049
3 27
r 8__
1014
:
Sul
fate
.
635
e I
Non
e
__-
---
Tot
al D
isso
lved
Sol
ids
"-
- N
one
- -__
s.
_ 2 i
- _
-_-n
e '
_ -
Alk
alin
ity a
s C
aCO
3 -
- N
one
CC
GC
04E
6 28
/Aug
/201
4 B
icar
bona
te
261
l =
N
one
__G
C _0
43'_
28
/Aug
/201
4 C
alci
um
69
CC
GC
04
T6
28/A
ug/2
014
Chl
orid
e 82
i
=
Non
e
CC
GC
-'_
28
/Aug
/201
4 H
ardn
ess
as C
aCO
3 27
1 N
one
-_. -
-_
_ 00
00_
_.
.. .C
CG
C
CC
GC
__
CC
GC
-3
28
/Aug
/201
4 M
agne
sium
-
D
:CG
C
0496
28
/Aug
/201
4 N
itrai
+
Nitr
ite a
s N
=
N
one
CC
GC
_049
6 28
/Aug
/201
4 N
itrat
e as
NO
3 -N
'_
S
_
Non
e --
'_
-CG
C
04
`_
28/A
ug/2
014
Nitr
ite a
s N
O2N
0.
4 =
_I N
one
- -,
CC
GC
:CG
C
04
=
28/A
ug/2
014
Pot
assi
um
2.9
_ D
:CG
C 0
465
2 3
-.8-
_r.'.
7:::
s: am
56
=
D
GC
04
r_
- -_
__
_ _f
cCa
-___
...
753
CC
GC
04
=3
- -, _
_ -
__ f
ate
32
= C
GC
_048
.6
/Aug
/"-=
-_
I Dis
solv
ed S
olid
s
- CG
C = -=
_ __
/Aug
/___
- .2
c_l
inity
as
CaC
O3
232
,
CC
GC
_"
??
28 /A
ug/2
014
Bic
arbo
nate
34
2
CC
GC
S
=
28/A
ug/2
014
Cal
cium
-
148
/Aug
/C_-
_
brid
e 23
0
/Aug
/2 =
_ -s
-dne
as a
s C
ac03
64
1 :
:CG
C 0
41+
.1
2 1r
2_
_ M
agne
sium
66
CC
GC
04
56
.cra
te+
Nitr
ite a
s N
12
_CG
C
__
cmte
as
NO
3_N
11
? _C
GC
_043
3 28
/Aug
/201
4 N
itrite
as
NO
2-N
CC
GC
= EE
=
3/A
ug/2
014
Pot
assi
um
:CG
C 7
=9S
:S
/Aug
/201
4 S
odiu
m
221
_.__
. _.._
. .._
_.__
:C
GC
04
E
:S/A
ug/2
014
Spe
<ifK
Ond
uctr
viry
20
78
:CG
C 04
-5
_/A
UgJ
_==
=
c_ f
ate
461
:CG
C 0
496
23/A
ug/2
-1-
-_ =
lDis
solv
edS
olid
s 14
17
Non
e
Non
e
Non
e '
Non
e N
one
D Non
e N
one
D
Non
e N
one
Non
e
D
D
Non
e
Non
e N
one
Non
e C
CG
C_0
5}=
__
-_=
_=4
Alk
alin
ity a
sCaC
O3
211
:
FIA
é,d?
yo,
{ R
éSgñ
al
l C
CG
C_0
500
28/A
ug/2
014
Bic
arbo
nate
C
CG
C 05
00
28 /A
ug/2
014
Cal
cium
17
1 =
_
-..._
C
CG
C
- C
CG
C 05
00
28/A
ug/2
014
Chl
orid
e 26
0 =
,
Non
e C
CG
C 05
00
28 /A
ug/2
014
l H
ardn
ess
as C
aCO
3 74
4
CC
GC
05
00
28/A
ug/2
014
Mag
nesi
um
CC
GC
05
00
28 /A
ug/2
014
G
Nitr
ate
+ N
itrite
as
N
= --
C
CG
C
CC
GC
05
00
28/A
ug/2
014
Nitr
ate
as N
O3 -
N
CC
GC
05
00
28/A
ug/2
014
Nitr
ite a
s N
O2
-N
0.3
_CC
GC
CC
GC
_050
0 __
28/A
Ug/
2014
P
otas
sium
4.
8
CC
GC
_050
0 28
/Aug
/201
4 S
odiu
m
170
_
CC
GC
05
00
28 /A
ug/2
014
Spe
cific
Con
duct
iviry
20
63
Non
e
CC
GC
_050
0 28
/Aug
/201
4 S
ulfa
te
273
e N
one
CC
GC
05
00
28 /A
ug/2
014
Tot
al D
isso
lved
Sol
ids
1331
=
N
one
CC
GC
_050
2 28
/Aug
/201
4 I
Alk
alin
ity a
s C
aCO
3 26
9 C
CG
C__
C
CG
C 05
02
28/AUg/2014
Bicarbonate
328
=
'brie
'
CC
GÇ
0502
28
/Aug
/201
4 C
alci
um
- -'
CC
GC
._
._
CC
GC
_.
CC
GC
_
CC
GC
05
02
28/A
ug/2
01 4
Chl
orid
e E
S
%.t
e
CC
GC
. 050
2 28
/Aug
/201
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4 O
xida
tion-
Red
uctio
n P
oten
tial
179.
1 m
V
_ C
CG
C_0
175
14/M
ar/2
014
Oxy
gen,
Dis
solv
ed
7.69
m
g/L
CC
GC
_017
5 14
/Mar
/201
4 pH
__
_ 7.
21
none
CC
GC
01
75
14/M
ar/2
014
Spe
cific
Con
duct
ivity
19
50
'Wan
C
CG
C
0175
14
/Mar
/201
4 T
empe
ratu
re
15.3
D
eg C
CC
GC
01
76
14/M
ar/2
014
Oxi
datio
n-R
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tion
Pot
entia
l 11
0.5
mV
,
CC
GC
01
76
14/M
ar/2
014
Oxy
gen,
Dis
solv
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8.77
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CC
GC
01
76
14/M
ar/2
014
pH
7.91
'
none
CC
GC
01
76
14/M
ar/2
014
, S
peci
ficC
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1910
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GC
01
76
14/M
ar/2
014
'
Tem
pera
ture
17
.9
, D
eg C
CC
GC
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7 14
/Mar
/201
4 O
xida
tion-
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uctio
n P
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tial
1572
.
mV
C
CG
C
0177
14
/Mar
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4 O
xyge
n, D
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lved
1.
76
, m
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CC
GC
01
77
14/M
ar/2
014
pH
7.28
no
ne
.
CC
GC
01
77
14/m
ar/2
014
Spe
cific
Con
duct
ivity
15
04
. uS
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CC
GC
_017
7 14
/Mar
/201
4 T
empe
ratu
re
15.4
.
Deg
C
CC
GC
01
78
12/M
ar/2
014
Oxi
datio
n-R
educ
tion
Pot
entia
l
18.4
D
egC
2640
m
V
006C
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5 27
/Aug
/201
4 O
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uctio
n P
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tial
145
1 m
V
CC
GC
01
78
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0060
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014
Oxy
gen,
Dis
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10.8
9 m
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60_0
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12/M
ar/2
014
pH
7 no
ne
CC
GC
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8 27
/Aug
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4 pH
6.
77
[
none
CC
GC
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8 12
/Mar
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4 S
peci
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ity
774
i uS
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CC
GC
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8 27
/Aug
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4 S
peci
ficC
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ctiv
ity
702
us/c
m
.1
CC
GC
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8 12
/Mar
/201
4 '
Tem
pera
ture
15
.5
Deg
C
.
0060
_017
8 27
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4 T
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C
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9 12
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4 .
Oxi
datio
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Pot
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l 13
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0080
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9 12
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4 O
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pH
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CG
C 01
79
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014
Spe
cific
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16
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CC
GC
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79
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pera
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16
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GC
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Oxi
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Pot
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l 11
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GC
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80
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ar/2
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pH
7.36
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80
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014
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62
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17
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81
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l 14
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CC
GC
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81
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pH
7.35
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81
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014
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69
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GC
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81
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pera
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18
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82
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2 13
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pH
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CC
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2 13
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GC
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014
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datio
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V
CC
GC
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3 13
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4 .
Oxy
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GC
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3 13
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4 1
pH
7.45
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CC
GC
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3 13
/Mar
/201
4 S
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1306
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GC
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3 13
/Mar
/201
4 T
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20.3
D
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CC
GC
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4 13
/Mar
/201
4 O
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181.
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V
CC
GC
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4 13
/Mar
/201
4 O
xyge
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2.
76
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L C
OG
C_0
184
13/M
ar/2
014
pH
7.6
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CC
GC
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4 13
/Mar
/201
4 S
peci
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ity
713
uS/c
m
CC
GC
_018
4 13
/Mar
/201
4 T
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ratu
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18.9
D
egC
CC
GC
_018
5 13
/Mar
/201
4 O
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n P
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184.
5 un
V
CC
GC
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5 13
/Mar
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4 O
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2
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L C
CG
C 01
85
13/M
ar/2
014
PH
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6 no
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CC
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13
/Mar
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4 S
peci
ficC
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906
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m
CC
GC
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5 13
/Mar
/201
4 T
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ratu
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18.5
D
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C
CG
C_0
186
14/M
ar/2
014
Oxi
datio
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educ
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Pot
entia
l 13
0.6
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CC
GC
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6 14
/Mar
/201
4 O
xyge
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5.
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14/M
ar/2
014
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GC
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6 14
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'
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11
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CC
GC
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6 14
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15.2
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Pot
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CC
GC
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7 14
/Mar
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7.
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7.14
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CC
GC
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7 14
/Mar
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4 S
peci
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2185
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GC
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7 14
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4 T
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15.2
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188
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8 19
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4 pH
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8 19
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4 S
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8 19
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4 T
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153
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CC
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9 19
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124.
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CC
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9 1
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014
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9 19
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44
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9 19
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4 T
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15.6
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190
19/M
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V
CC
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6.
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4 pH
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44
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GC
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/Mar
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4 S
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442.
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0 19
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17.6
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1 19
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1 19
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1 19
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19
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3 19
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4 19
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4 19
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HT -1212 110528 10/25/13 1/11/14 CCGC_0313 5.6 +/- 0.4 0.0 +/. 28.9 mixed
large component of terrigenic helium
causes e4 /'He age uncertainty. He
predicted age of old component: 5000 yrs
HT -1213 110529 10/25/13 1/13/14 CCGC_0013 4.6 +1- f 7 modern or
mixed submitted for 3T /3He only
HT -1214 110530 10/24/13 1/13/14 CCGC_0019 51 +/- 0.6 18.9 +/- 1.9 modern submitted-for 3T/3He only
HT -1215 110531 10/24/13 1/13/14 00000026 4.2 4/- 0.3 50.0 +/- 11.7 mixed
Large cómponent of terrigenic helium
causes 'H/tHe age uncertainty. °He
predicted age of old component: 30000 yrs
HT -1216 110532 10/24/13 1/13/14 CCGC_0029 5.9 +/- 0.9 0.0 +/- 14.4 modern samples flows sign" helium loss canning
H /sHe age uncertainty.
HT -1217. 110533 10/24/13 1/13/14 CCGC_0030 4.0 +/- 2.1 19.0 25.0 mixed High 3H error and terrigenic helium cause
high age uncertainty.
HT -1218 110534 10/24/13 1/13/14 CCGC_0034 1.5 +/- 0.3 modemor
mixed submitted for3T /3He only
HT -1219 I0 10/21/13 1/13/14 CCGC_0035 6.7 +/- 0.4 modern or
mixed submitted for 3T /3He only
HT -1220 110536 10/21/13 1/13/14 CCGC_0035 6.5 4/- 0.4 - modern or
mixed submitted for 3T /3He only
HT- 1221 110537 10/25/13 1/13/14 CCGC_0058 5.9 4/- 0.4 52.7 +/- 6.4 mixed
Large component of terrigenic helium
ceases 3H /He age uncertainty. °He
predicted age of old component: 30000 yrs
HT-1222 110538 10/23/13 1/13/14 CCGC_0062 6.6 '4/- 0.6 0.0 +/- 1.7 modern
HT -1223 110539 10/21/11 1/13/14 C000 0070 1.0 +/- 0.5 modern submitted for 3T /3He only
Data Release CFC14 -01, Job # CFC0126
Client ID
Recharge Age
in years before sampling date
CFC12 error CFC11 error years years
CFC13
years
error
CCGC_0002 43 2 45 2 39 2
CCGC_0002 43 2 44 2 40 2
CCGC_0002 43 2 44 2 40 2
CCGC_0004 51 2 52 2 45 2
CCGC_0004 50 2 51 2 44 2
CCGC_0004 50 2 51 2 45 2
CCGC_0013 42 2 53 2 46 2
CCGC_0013 42 2 52 2 44 2
CCGC_0013 42 2 54 2 46 2
CCGC_0019 Supersaturated Supersaturated 30 2
CCGC_0019 Supersaturated Supersaturated 30 2
CCGC_0019 Supersaturated Supersaturated 30 2
CCGC_0023 56 2 56 2 46 2
CCGC_0023 57 2 58 2 49 2
CCGC_0023 55 2 55 2 48 2
CCGC_0026 Supersaturated Supersaturated 27 2
CCGC_0026 Supersaturated Supersaturated 28 2
CCGC_0026 Supersaturated Supersaturated 27 2
CCGC_0029 Supersaturated Supersaturated 27 2
CCGC_0029 Supersaturated Supersaturated 28 2
CCGC_0029 Supersaturated Supersaturated 28 2
CCGC_0030 Supersaturated Supersaturated 27 2
CCGC_0030 Supersaturated Supersaturated 27 2
CCGC_0030 Supersaturated Supersaturated 27 2
CCGC_0034 46 2 53 2 46 2
CCGC_0034 45 2 53 2 45 2
CCGC_0034 45 2 53 2 47 2
CCGC_0035 47 2 55 2 47 2
CCGC_0035 48 2 55 2 48 2
CCGC_0035 47 2 55 2 48 2
CCGC_0058 28 2 41 2 37 2
CCGC_0058 28 2 40 2 36 2
CCGC_0058 28 2 39 2 35 2
CCGC_0060 39 2 51 2 43 2
CCGC_0060 39 2 51 2 43 2
CCGC_0060 39 2 51 2 43 2
CCGC_0070 59 2 58 2 49 2
CCGC_0070 61 2 59 2 51 2
CCGC_0070 62 2 60 2 50 2
Supersaturated indicates there are additional non- atmospheric source(s) of the CFC, making a valid age determination impossible.
Appendix E -- Exceedence Notification Follow -Up Report
The CCGC is currently seeking permission from members to display this information on a well -by -well basis. This information will be provided in the complete Groundwater Characterization Report.
ATTACHMENT 7
January 26, 2015
Mr. Kenneth A Harris Jr., Executive Officer Central Coast Regional Water Quality Control Board
895 Aerovista Place, Suite 101
San Luis Obispo, CA 93401 -7906
Dear Mr. Harris,
The Central Coast Groundwater Coalition (CCGC) is submitting a response to
the Staff Report for Regular Meeting of January 29 -30, 2015, Item 16. The subject
of this item is "Irrigated Lands Regulatory Program - Water Board Review of the
Manner in Which Central Coast Groundwater Coalition Groundwater Testing
Results are Disclosed to the Public ".
The CCGC believes that the Staff Report is incorrect in the characterization of
the CCGC approach to reporting the concentration of nitrate in groundwater in
the Central Coast groundwater basins. To correct the misrepresentations, the
CCGC is submitting comments to be included in the material that is distributed
to the Regional Water Board. In addition, CCGC representatives will discuss the
CCGC responses during a presentation at the upcoming Regional Water Board
meeting.
Thank you for the opportunity to provide comments to the Regional Water
Board.
Thank you,
D
Parry Klassen Executive Director
Central Coast Groundwater Coalition 512 Pajaro Street Salinas CA 93901
(831) 585 -1435 centralcoastgc.org
Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
ATTACHMENT 7
Dear Mr. Harris,
The CCGC appreciates the opportunity to respond to the Staff report for the January 29 - 30th Central Coast Regional Board meeting. Included in this letter are general comments, specific narrative comments and responses to Regional Board staff comments specific to thé contour maps (Table 2 of Item 16 in the Staff Report).
First the CCGC would like to clarify the purpose of the contour maps as described the Northern Counties Workplan. Regional Board staff imply that characterization across the entire region is inadequate. But as
indicated below, the CCGC is required to characterize groundwater quality in the immediate vicinity of member parcels. The language from the Order (Attachment A) is provided below.
"In lieu of conducting individual groundwater monitoring, Dischargers may participate in a cooperative groundwater monitoring effort to help minimize costs and to develop an effective groundwater monitoring program. Qualifying cooperative groundwater monitoring and reporting programs may include, but are not limited to, regional or subregional groundwater programs developed for other purposes as long as the proposed cooperative groundwater monitoring program meets the Central Coast Water Board's general purpose of characterizing groundwater quality and ensuring the protection of drinking water sources. Proposals for cooperative groundwater monitoring efforts, including the use of other regional or subregional groundwater monitoring programs must be approved by the Executive Officer. At a minimum, the cooperative groundwater monitoring effort must include sufficient monitoring to adequately characterize the groundwater aquifer(s) in the local area of the participating Dischargers characterize the groundwater quality of the uppermost aquifer, and identify and evaluate groundwater used for domestic drinking water purposes. Cooperative groundwater monitoring efforts must comply with the requirements for sampling protocols and laboratory analytical methods identified in this MRP, including parameters listed in Table 3, or propose a functional equivalent that meets the same objectives and purposes as individual groundwater monitoring. The cooperative groundwater monitoring program must report results consistent with individual groundwater reporting defined in part 2.B, or report results in a manner that is consistent with that approved by the Executive Officer in his or her approval of the cooperative groundwater monitoring proposal. Dischargers electing to participate in a cooperative groundwater monitoring effort must convey this election to the Central Coast Water Board within 90 days of adoption of this Order, and the individual groundwater monitoring requirements shall not apply as long as a cooperative groundwater monitoring proposal for that Discharger's area is submitted within one (1) year of adoption of this Order. If no cooperative groundwater monitoring proposal for that Discharger's area is submitted within one (1) year, then the individual groundwater monitoring provisions shall apply and the Discharger shall have one (1) year to comply with the provisions identified in Part 2."
CCGC Response to Staff Report January 26, 2015 Page 2 of 14
Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
CCGC Response to Staff Report_ Corn I<n eiï f=s
General Comments The CCGC has 5 general comments regarding the Staff report. In addition to these overarching comments, the CCGC is responding to the narrative comments and has inserted a table with the CCGC
responses for each of the Tech Memo staff comments received regarding the contour maps.
1. The criticisms of the CCGC analysis are premature. Judgments of the contour maps should
appropriately be delayed until after the delivery and staff review of the characterization report.
The staff seems to imply that the CCGC has manipulated or excluded data to obtain a higher level
of compliance with the nitrate MCL. Explanations of why wells were excluded are provided in
both tech memos and no criticism of those explanations were provided by staff for the second
technical memorandum. The two contour maps are a result of the addition of more data to the analysis and revised methodology described in the tech memo and correspondence with Regional
Board staff.
2. The staff report misrepresents the requirements of the Order by stating that the CCGC needed to characterize groundwater quality in agricultural areas (p3 of staff report). In fact, the Order states: As stated in the background section above, "at a minimum, the cooperative groundwater monitoring effort must include sufficient monitoring to adequately characterize the groundwater aquifer s in the local area of the artici.atin: Dischar:ers characterize the : roundwater .ualit. of the uppermost aquifer, and identify and evaluate groundwater used for domestic drinking water purposes." This means that the CCGC characterization effort does not need to have high
confidence in the contour lines across the entire region, particularly in areas with few members.
3. The staff report misrepresents that the CCGC could have found additional wells to supplement the data and analyses in the tech memos. During discussions with staff on the morning of November 17, 2014 at Regional Board Offices in San Luis Obispo John Robertson stated that they could not find additional wells to sample and they could not therefore request that the CCGC find additional wells.
4. There appears to be confusion on the part of the staff with respect to the relationship between the standard deviations and confidence intervals and the interpretation of those terms. There is
clearly a level of confidence that can be assigned based on the calculated standard deviation estimates. This has been represented in maps presented in the second Technical Memorandum.
It is unclear what criteria staff is using to reject or accept the contour maps. CCGC consultants opine that the degree to which the mapped concentrations agree with measured concentrations should be the primary criterion. Appendix A and additional information provide below show the consistent agreement of predicted concentrations with measured concentrations in samples
collected by multiple entities including the CCGC and in GeoTracker.
5. The CCGC submits that decisions to accept or reject contour maps should be based on the final
maps to be presented in the Characterization Report. The technical memoranda were intended to provide progress updates.
CCGC Response to Staff Report January 26, 2015 Page 3 of 14
Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
Narrative Comments In addition to the above, below are responses to the narrative comments made in the Staff Report. RB = Regional Board staff comments. CCGC - CCGC response to comments.
RB: Contour maps, because of the decision-making that goes into drawing contours where data is sparse, are interpretations of the data.
CCGC: Using kriging, there is no subjective decision making that goes into drawing the contours. The semi-variogram model is selected based on the spatial distribution of the data and therefore is adjusted to optimize the fit as was done for this case. The contours were not hand-drawn based on some subjective interpretation but a grid of values was generated by the kriging program. The result of the fit for 581 points in the Salinas Valley is shown in Figure 2. For any mapping method, there is uncertainty associated with areas where there are no wells. We quantified this uncertainty by mapping the standard deviation and creating maps with varying confidence levels.
RB: In general, the level of precision and accuracy of such interpretations increases with the amount of data available. In addition, precision and accuracy of such interpretations generally decreases when the hydrogeology is complex or highly variable.
CCGC: Agreed.
RB: The CCGC contour maps provided on April 30, 2014 and December 10, 2014 provide two very different interpretations based upon similar data, and in many cases the contour maps do not coincide with the actual data (see Attachment 3).
CCGC: In the December 10 version, over 100 additional data collected by the CCGC and individuals were used to map nitrate concentrations. Also, a different kriging model was used. This resulted in an improved mapping of nitrate concentrations as demonstrated by Appendix A and Figures 1 and 2 below. Moreover, in the interest of conservatism, we used the maximum value where there were multiple concentrations (in samples collected with time) and coincident points. For the first technical memorandum, we used the average value.
RB: For example, in areas where there are only a few wells with very different nitrate concentrations and a large distance between wells, the decision regarding how to interpret the contour interval is very subjective.
CCGC: Subjectivity implies that there is some decision to create a map a certain way. This is not the case because kriging uses a semi-variogram model based on the existing data that estimates concentrations between known points. We attempted to optimize this model to map nitrate concentrations shown in the December 10 version and is illustrated in Figure 2.
RB: The difference in interpretation is also evident in the tables describing the statistics. The version submitted on April 30, 2014, indicates that the percent of the Salinas Valley map as over the drinking water standard is 58%; while the version submitted on December 10, 2014, indicates only 28% over the drinking water standard. There are similar differences for the statistics reported for the subbasins; for example the Eastside
CCGC Response to Staff Report January 26, 2015 Page 4 of 14
Item 16 Public Comment 2
January 29-30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
subbasin is reported as 83% and 54 %, respectively, over the drinking water standard for the April 30, 2014 and December 10, 2014, versions.
CCGC: As described above, we refined our methods and used additional data in the second version of the maps.
RB: While the Revised Tech Memo for Salinas Valley submitted on December 10, 2014,
includes information regarding the probability that wells in certain contours exceed the drinking water standard, the Revised Tech Memo does not provide any information regarding the certainty of the contour maps or the probability that the interpreted results are correct. For example, the CCGC contour maps shown in Attachment 3 include a
contour interval of 36 - 45 mg /L Nitrate as NO3. What is the confidence or probability that a well located in that contour interval actually falls within 36 - 45 mg /L Nitrate as
NO3?
CCGC: This is conveyed in the maps drawn at different confidence levels. At the 95% confidence level, any point within the area encompassing the 36 to 45 mg /L contour interval will be within the interval at 95% of the locations.
RB: As described above, the groundwater monitoring data reported to the Central Coast Water Board in compliance with the Agricultural Order may be interpreted and presented in a number of different ways. In cases where multiple interpretations are possible, it is
important for the public and stakeholders to have access to the underlying data to
evaluate the interpretation provided and to validate their own interpretations. Thus, staff concludes that the CCGC contour maps are not acceptable for providing reliable information to the public,
CCGC: As discussed above and as is shown in the report and Figure 2, the contours do provide useful information. When Michael Johnson, Parry Klassen and Steve Deverel met with Angela Shroeter, John Robertson and Hector Hernandez on November 17, 2014, staff stated that the maps are useful. While multiple interpretations are possible depending on assumptions about what wells to use in the mapping, we assert that the CCGC has done an excellent job of using the available data. Using the same data set and assumptions, mapping of areas of varying concentrations will not vary significantly
RB: In lieu of the actual groundwater data. In many areas, the CCGC contour maps do
not provide reliable information so that the public can make informed decisions related to
their drinking water quality and potential health exposure to nitrate. Additionally, staff also concludes that the CCGC contour maps do not provide reliable data for stakeholders to review characterizations of groundwater quality. Moreover, the contour maps would make it difficult for the public and other stakeholders to review the Central Coast Water Board's progress in identifying and prioritizing areas and individual farms that are at greater risk for pollutant loading and informing those domestic well users who may be affected by unsafe drinking water quality.
CCGC: The CCGC submits that there are two issues: the value of the contour maps and release of the data to the public. We have chosen to focus our responses on the former as this issue should be fully addressed and solidified prior to deciding on the need to disclose the data.
CCGC Response to Staff Report January 26, 2015 Page 5 of 14
Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
35'400El-
-.0 0 11
48
22103 3 ¡ it8 Am
6 c 4ós6I 7 1: *
8 49 1T 19
110 4 ll 4=6¡3
18 , 62
54 2
0(2) 1(9). 2(5). 4, 7(2). 8(3). 11(2). 12. 13. 14.(2). 16, 19(2), 20(2), 23. 25, 26(3). 27. 36, 40, 41(2) 45. 50. 63. 90, 284
2.4.6.7,8 :,8
Cet
0 42
1n : 59
1141, 126 ' 150
8 87 ¡ ;..,/1
115 4i
t 21' 300'15' 121'20r' W
L
Only wells used for nitrate mapping are shown Excluded wells include wets with known well depth greater than 400 feet or well use that is either irrigation or domestic /irrigation with unknown well depth
All NO't concentrations are rounded to the nearest integer.
LANGLEY AREA
.ff«rn
O
SEASIDE AREA
2_. 4
¡ (4 w
27 18 er s
.r r'
Al* . a:ii-.. .>r j, Pi
1 . ' .: tÁ '.. "l At .
.
71 j., _EAST SIDE SUBAREA
JI ;,69 2i . j, ,- ._
® 1i6 7ß 11¡`191 F' r.,^ r t3 , t9 t49 45 r ,'o
J
CORRAL DE 2; 4¡10 1 ' .1>:62g¡. 93. : :3 731i : .,; ;
TIERRA AREA , 8 1149 39 5
107 340 \. , . : . a
- z i .e `huatar
' r. " ,
281 3*! 26 26
Ç. 65 74! L9
7 74 44 35 28 -
r88 2 ` , 2, 151° - 13t 1 _
i711,35 ` 3 1
49 Gcnzefs 59 _
'50.
r.r
EXPLANATION
Neils with Mitrate Data
Estimated Nitrate Concentration m01L
< 22 5
n5-36 ( j3s -45
l..- 45.00
>90
Groundwater Besan
OO 3
1 i 1 1
Miles
+,.
PRESSURE SUBAREA
7 58 96
2}5
20
I. 97
The locations of CCGC member wells were randomly adjusted up to 0.5 miles in both the east -west and north -south directions to protect member privacy. The wells are plotted within a 1 mil block centered over the actual well location.
r - -
Sourcds: Esri. DeLorme USGS NPS Sources' E5i1 u. S21vn'n'w 121' Jnr tel'
-36'7G'0'N
Figure 1. Example comparison between mapped estimated nitrate concentrations and observed maximum nitrate concentrations for the Langley Area, East Side Aquifer, and Pressure Aquifer subbasins from the December 10 Technical Memorandum.
CCGC Response to Staff Report January 26, 2015 Page 6 of 14
Item 16 Public Comment 2 January 29 -30, 2015
Letter Central Coast Groundwater Coalition dated 1/26
600 -y --0:98-19x -- O:0548
R2 = 0.9978
500 --..
;` rtî 400 O Z -7) 300 co
ÿ 200 W
100
100 200 300 400
Measured NO3, mg /L
500 600
Figure 2. Relation of estimated and measured nitrate concentrations in the Salinas Valley.
CCGC Response to Staff Report January 26, 2015 Page 7 of 14
Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
Text of email exchange, Angela Schroeter (Regional Board staff) and Dave Leighton (Hydrofocus)
From: Schroeter, Angela @Waterboards < Angela .Schroeter @waterboards.ca.gov> Date: Mon, Dec 29, 2014 at 12:32 PM Subject: RE: Pajaro TM nitrate map To: Dave Leighton <leighton @hydrofocus.com> Cc: Steve Deverel <[email protected] >, "Robertson, John @Waterboards" < John .Robertson @waterboards.ca.gov >, "Hernandez, Hector @Waterboards" < Hector .Hernandez @waterboards.ca.gov> Dave - Thanks for your email. Our primary concern is related to the intervals >45 mg /L.. When the maximum can be 300+ mg /L, a top interval of >90 is not informative. The contour intervals should effectively inform the viewer about where the concentrations are increasing and where maximum concentrations exist, even above the MCL. If 10 mg /L intervals will not work, please let us know what you recommend. Thanks,
Angela From: Ieightonhf@ gmail.com [mailto:leightonhf©gmail.comj On Behalf Of Dave Leighton Sent: Tuesday, December 23, 2014 3:10 PM To: Schroeter, Angela @Waterboards Cc: Steve Deverel Subject: Pajaro TM nitrate map Hi Angela,
We are currently addressing comments on the Pajaro basin report and I have a question for you regarding the display of estimated nitrate concentrations. Comment 20 requests that we use a 10 mg /L contour interval below 45 mg/L and then a variable interval above 45 mg/L, depending on the data. We are concerned that too many colored intervals will make it difficult for the eye to perceive the differences. For the Salinas report we left the intervals below 45 mg /L as is and replaced the >45 interval with two intervals (45 -90 and > 90). Is this scheme adequate for the Pajaro report? I've attached an example map for Pajaro basin with these intervals. Thanks.
Dave Leighton HydroFocus, Inc. 530 -759 -2484
CCGC Response to Staff Report January 26, 2015 Page 8 of 14 Item 16 Public Comment 2
January 29 -30, 2015 Letter Central Coast Groundwater Coalition dated 1/26
Tab
le 1
. S
peci
fic C
CG
C re
spon
ses
to S
taff
com
men
ts fr
om T
able
2 o
f the
Sta
ff R
epor
t for
Item
16.
T
he fi
rst
thre
e co
lum
ns a
re r
epro
duce
d fr
om T
able
2.
Con
tour
Map
Crit
eria
Id
entif
ied
in J
uly
11,
2013
C
CG
C W
orkp
lan
App
rova
l
Sta
ff R
epon
ses
to
CC
GC
Con
tour
M
ap
Sub
mitt
ed
Apr
il 30
, 20
14
Sta
ff R
espo
nses
to
CC
GC
Con
tour
Map
S
ubm
itted
Dec
. 10
, 20
14
CC
GC
Res
pons
e
Con
ditio
n 10
: T
ech
Mem
o R
evis
ed T
ech
Mem
o de
scrib
es a
T
he w
ell d
ensi
ty v
arie
s w
ith th
e w
ells
sam
pled
in th
e va
rious
Sam
plin
g de
nsity
, re
solu
tion
and
acco
mpa
nyin
g co
ntou
r ra
nge
in w
ell d
ensi
ty fr
om 1
w
ell
loca
tions
with
in th
e C
entr
al C
oast
reg
ion.
T
he C
CG
C s
ampl
ed
scal
e m
ust
be s
uffic
ient
suc
h m
ap d
oes
not
incl
ude
per
25 a
cres
, to
1 w
ell
per
14
ever
y do
mes
tic w
ell f
rom
enr
olle
d pa
rcel
s an
d us
ed e
NO
1 da
ta
that
ind
ivid
ual
dom
estic
wel
l an
y in
form
atio
n to
ac
res
only
for
wel
ls w
here
the
fr
om th
e in
divi
dual
mon
itorin
g pr
ogra
m a
nd a
dditi
onal
dat
a
owne
rs th
at r
esid
e in
de
scrib
e w
ell
dens
ity o
r st
anda
rd d
evia
tion
was
less
th
an
desc
ribed
in t
he m
emor
anda
to d
evel
op t
he c
onto
urs
and
agric
ultu
ral
area
s w
ithin
the
to d
eter
min
e if
this
2.
5 m
g /L
NO
3.
The
R
evis
ed T
ech
char
acte
rize
the
qual
ity o
f sh
allo
w g
roun
dwat
er.
The
rel
evan
t
coop
erat
ive
grou
ndw
ater
de
nsity
is s
uffic
ient
. M
emo
does
not
des
crib
e th
e w
ell
issu
e is
the
dens
ity o
f wel
ls a
nd u
ncer
tain
ty in
the
vici
nity
of
mon
itorin
g pr
ogra
m b
ound
ary
Wel
l de
nsity
on
map
s de
nsity
for
all
wel
ls.
The
Rev
ised
m
embe
r pa
rcel
s, n
ot a
cros
s th
e en
tire
regi
on.
can
mak
e in
form
ed d
ecis
ions
ap
pear
s sp
arse
in s
ome
Tec
h M
emo
indi
cate
s th
at t
he
rela
ted
to t
heir
drin
king
wat
er
area
s.
wel
l de
nsity
va
lues
app
ear
Mor
eove
r, t
he s
tate
men
t th
at w
ell d
ensi
ty is
suf
ficie
nt is
bas
ed
qual
ity a
nd p
oten
tial h
ealth
ge
nera
lly s
uffic
ient
for
map
ping
on
agr
eem
ent w
ith m
easu
red
and
estim
ated
val
ues
as s
how
n
expo
sure
to n
itrat
e.
of a
reas
w
here
gro
undw
ater
is
likel
y to
be
over
M
CL.
How
ever
, th
ere
is n
o ev
alua
tion
of w
heth
er t
he w
ell d
ensi
ty is
suffi
cien
t giv
en th
e sp
atia
l
varia
bilit
y of
the
and
spec
ific
loca
l con
ditio
ns.
in f
igur
es i
n A
ppen
dix
A.
(Als
o, s
ee e
xam
ple
figur
e be
low
,
Fig
ure
1).
Spe
cific
ally
, w
e sh
ow m
aps
with
pos
ted
nitr
ate
conc
entr
atio
ns a
nd c
ompa
rison
s w
ith G
eoT
rack
er v
alue
s. A
s
stat
ed in
the
rep
ort,
ther
e is
ver
y go
od a
gree
men
t. M
oreo
ver,
he
rein
in F
igur
e 2,
we
prov
ide
an e
xam
ple
com
paris
on o
f m
easu
red
vs. pr
edic
ted
valu
es fo
r 581
poi
nts
in th
e S
alin
as
Val
ley
that
will
be
incl
uded
in t
he C
hara
cter
izat
ion
Rep
ort.
The
geos
tatis
tical
mod
el p
redi
cts
mea
sure
d va
lues
with
in p
lus
or
min
us 0
.2 m
g/L
or 0
.03%
of
the
rang
e of
mea
sure
d va
lues
(bas
ed o
n th
e ca
lcul
atio
n of
the
root
mea
n sq
uare
err
or)
for
the
rang
e fo
r co
ncen
trat
ions
fro
m l
ess
than
det
ectio
n to
ove
r
600
mg
/L.
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
, 20
15
Pag
e 9
of 1
4
Item
16
Pub
lic C
omm
ent
2
Janu
ary
29 -3
0,
2015
Le
tter
Cen
tral
C
oast
Gro
undw
ater
Coa
litio
n da
ted
1/26
Con
tour
Map
Crit
eria
Id
entif
ied
in J
uly
11,
2013
C
CG
C W
orkp
lan
App
rova
l,
Sta
ff R
epon
ses
to
CC
GC
Con
tour
M
ap S
ubm
itted
A
pnl3
0, 2
014
Sta
ff R
espo
nses
to
CC
GC
Con
tour
Map
S
ubm
itted
Dec
10
, 20
14
CC
GC
Res
pons
e
Con
ditio
n 10
: T
ech
Mem
o st
ates
that
C
onto
ur m
aps
stat
e th
at w
ells
T
he r
atio
nale
for
sele
ctin
g th
e up
per 4
00 fe
et is
sta
ted
in th
e C
onto
ur m
aps
mus
t cha
ract
eriz
e da
ta fo
r w
ells
that
are
w
ith d
epth
s gr
eate
r th
an 4
00
repo
rt.
We
revi
ewed
and
pro
cess
ed o
ver 3
,000
wel
l log
s to
gr
ound
wat
er n
itrat
e co
ncen
trat
ions
sh
allo
wer
than
400
fe
et a
re e
xclu
ded.
C
onto
ur
dete
rmin
e th
at t
he la
rge
maj
ority
of o
ver
1,50
0 do
mes
tic w
ell
at s
peci
fic d
epth
, fo
cus
on s
hallo
w
feet
-are
use
d to
m
aps
do n
ot s
peci
fical
ly
com
plet
ion
repo
rts
in th
e S
alin
as V
alle
y ar
e co
mpl
eted
with
in
grou
ndw
ater
, an
d in
dica
te d
epth
re
pres
ente
d on
the
map
. de
velo
p co
ntou
r m
aps,
but d
epth
ran
ge i
s no
t in
dica
ted
on t
he
cont
our
map
.
desc
ribe
the
180
foot
aqu
ifer
or
disc
reet
aqu
ifer z
ones
.
400
feet
of l
and
surf
ace.
M
oreo
ver,
gro
undw
ater
with
in 4
00
feet
of l
and
surf
ace
is g
ener
ally
con
side
red
shal
low
gr
ound
wat
er.
In th
e in
tere
st o
f fir
st c
hara
cter
izin
g th
e do
mes
tic s
uppl
y w
ater
and
sec
ond
the
shal
low
gro
undw
ater
w
e se
lect
ed 4
00 fe
et a
s th
e de
pth
of g
roun
dwat
er fo
r m
appi
ng.
(See
pag
es 1
0 an
d 24
-31
for t
he h
ydro
logi
c co
ntex
t di
scus
sion
and
for
info
rmat
ion
abou
t wel
l com
plet
ion
repo
rt
dept
hs)
-
We
disc
usse
d th
e aq
uife
rs in
the
Sal
inas
Val
ley
whi
ch a
re
limite
d in
ext
ent p
rimar
ily to
the
Pre
ssur
e, n
orth
ern
For
ebay
an
d pa
rts
of th
e E
asts
ide
subb
asin
s.
The
aqu
ifer
delin
eatio
ns
are
of fi
rst o
rder
im
port
ance
for
drin
king
wat
er th
roug
hout
th
e V
alle
y be
caus
e th
e "c
onfin
ing
zone
s se
para
ting
aqui
fers
ar
e no
t. co
ntin
uous
. M
oreo
ver,
Fog
g an
d ot
hers
' de
mon
stra
ted
that
the
trad
ition
al v
iew
of
dist
inct
aqu
atar
ds
and
aqui
fers
in
the
Sal
inas
Val
ley
is m
ore
appr
opria
tely
vi
ewed
as a
het
erog
eneo
us m
ixtu
re a
nd l
ayer
ing
of
perm
eabi
lity.
We
ther
efor
e de
emed
it m
ore
appr
opria
ted
to
use
a de
pth
inte
rval
rat
her t
han
spec
ific
aqui
fers
.
I F
ogg,
G.
E.,
LaB
olle
, E
. M
., an
d W
eiss
man
n, G
. S
., 19
99. G
roun
dwat
er v
ulne
rabi
lity
asse
ssm
ent:
Hyd
rolo
gic
pers
pect
ive
and
exam
ple
from
Sal
inas
V
alle
y, C
alifo
rnia
, A
sses
smen
t of
Non
-Poi
nt S
ourc
e P
ollu
tion
in t
he V
ados
e Z
one
(Geo
phys
ical
Mon
ogra
ph 1
08).
Am
eric
an G
eoph
ysic
al U
nion
.
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
; 20
15
Pag
e 10
of 1
4
Item
16
Pub
lic C
omm
ent 2
Janu
ary
29-3
0, 2
015
Lette
r C
entr
al C
oast
Gro
undw
ater
Coa
litio
n da
ted
1/26
Con
tour
Map
Crit
eria
Id
entif
ied
in J
uly
11,
2013
C
CG
C W
orkp
lan
App
rova
l -r.
Sta
ff R
epon
ses
to
- C
CG
C C
onto
ur
Map
Sub
mitt
ed
Apr
il 30
, 20
14
Sta
ff R
espo
nses
to
CC
GC
Con
tour
Map
S
ubm
itted
Dec
10
, 20
14
CC
GC
Res
pons
e
Con
ditio
n 10
: N
o ad
ditio
nal
sam
plin
g S
ame
as A
pril
30, 20
14,
Eve
ry d
omes
tic s
uppl
y w
ell o
n ev
ery
mem
ber
The
ana
lysi
s w
ill b
e pe
rfor
med
to
was
atte
mpt
ed o
r ve
rsio
n.
parc
el w
as s
ampl
ed (
with
the
exc
eptio
n of
7 w
ells
achi
eve
the
high
est
leve
l of
su
gges
ted
to i
ncre
ase
on p
rope
rtie
s th
at w
ould
not
gra
nt a
cces
s (o
f tho
se
cert
aint
y po
ssib
le w
ith t
he w
ells
co
nfid
ence
or
conf
irm
7 w
ells
, 6
will
be
sam
pled
in A
pril
2015
).
Tha
t
that
are
sel
ecte
d fo
r sa
mpl
ing,
an
d th
e an
alys
is w
ill e
xplic
itly
prov
ide
the
conf
iden
ce
valu
e fo
r
adeq
uacy
of
cont
ours
. C
CG
C m
embe
rs m
ay
have
num
erou
s
mea
ns e
very
dom
estic
wel
l tha
t co
uld
be s
ampl
ed
was
sam
pled
.
any
loca
tion
on t
he m
ap.
If th
e irr
igat
ion
and
drin
king
A
dditi
onal
wel
ls c
ould
not
be
iden
tifie
d by
the
CC
GC
det
erm
ines
tha
t the
re a
re
wat
er w
ells
on
thei
r C
CG
C.
In d
iscu
ssio
ns w
ith R
egio
nal
Boa
rd s
taff
in
mor
e w
ells
that
may
be
sam
pled
pr
oper
ty.
For
the
San
Lu
is O
bisp
o on
the
mor
ning
of
Nov
embe
r 17
in
in o
rder
to a
chie
ve a
hi
gher
S
alin
as V
alle
y, s
ampl
ing
Reg
iona
l Boa
rd o
ffice
s, J
ohn
Rob
erts
on s
tate
d th
at
conf
iden
ce i
nter
val,
they
mus
t fo
cuse
d on
onl
y R
egio
nal B
oard
sta
ff co
uld
not
iden
tify
addi
tiona
l
imm
edia
tely
inf
orm
the
Exe
cutiv
e do
mes
tic d
rinki
ng
wel
ls to
sam
ple
and
coul
d no
t pl
ace
that
bur
den
on
Offi
cer
and
pres
ent
a pl
an,
incl
udin
g sc
hedu
le, f
or a
dditi
onal
wat
er w
ells
- no
addi
tiona
l sam
plin
g
the
CC
GC
. T
he C
CG
C u
sed
data
fro
m a
ll ad
ditio
nal
wel
ls th
at c
ould
be
iden
tifie
d an
d fo
r whi
ch
sam
plin
g as
app
ropr
iate
, to
be
from
irr
igat
ion
wel
ls
suffi
cien
t co
nstr
uctio
n in
form
atio
n w
as a
vaila
ble
to
appr
oved
by
the
Exe
cutiv
e w
as a
ttem
pted
to
allo
w th
e w
ell t
o be
ass
igne
d to
a de
pth
of 0
-400
O
ffice
r.
assi
st w
ith
grou
ndw
ater
ch
arac
teriz
atio
n or
ft.
As
stat
ed o
n pa
ges
22 -2
3 of
the
Dec
embe
r 10
Con
ditio
n 11
: de
velo
pmen
t of
T
echn
ical
Mem
oran
dum
, irr
igat
ion
wel
ls a
nd
The
CC
GC
mus
t in
clud
e ad
ditio
nal
cont
our
map
s.
In
irrig
atio
n /do
mes
tic w
ell w
ere
cons
ider
ed to
be
sam
plin
g fo
r us
e as
a va
lidat
ion
addi
tion,
wel
ls m
ay
deep
er th
an 4
00 fe
et.
Thi
s w
as b
ased
on
data
set
to c
onfir
m a
dequ
acy
of
also
exi
st i
n th
e in
form
atio
n ob
tain
ed in
the
fie
ld a
nd w
ell
cont
ours
. pr
ogra
m a
rea
that
do
not b
elon
g to
CC
GC
mem
bers
but
are
av
aila
ble
for s
ampl
ing.
com
plet
ion
repo
rts.
The
se ad
ditio
nal d
ata
poin
ts c
ould
ass
ist t
o in
crea
se c
onfid
ence
or
conf
irm a
dequ
acy
of
cont
ours
. C
CG
C d
id n
ot
brin
g ad
ditio
nal
wel
ls
to th
e at
tent
ion
of th
e E
xecu
tive
Offi
cer.
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
, 20
15
Pag
e 11
of
14
Item
16
Pub
lic C
omm
ent
2
Janu
ary
29 -3
0, 2
015
Lette
r C
entr
al C
oast
Gro
undw
ater
Coa
litio
n da
ted
1/26
Con
ditio
n 11
: C
onfid
ence
inte
rval
s ar
e K
riged
nitr
ate
conc
entr
atio
n T
he t
erm
ra
nge
of c
onfid
ence
inte
rval
" is
not
com
mon
ly u
sed
Any
con
tour
map
s pr
oduc
ed m
ust
not
addr
esse
d in
the
map
s ar
e id
entif
ied
as e
stim
ated
an
d it
is n
ot c
lear
wha
t it
mea
ns.
The
CC
GC
did
not
pro
vide
in
clud
e th
e co
nfid
ence
int
erva
l for
re
port
or
cont
our
map
s.
valu
es,
but
do n
ot i
nclu
de a
ny
conf
iden
ce i
nter
vals
for
con
tour
s as
it is
im
poss
ible
to d
o th
is
estim
ated
val
ues.
Con
tour
map
K
riged
nitr
ate
info
rmat
ion
rega
rdin
g ra
nge
of
on a
tw
o- di
men
sion
al m
ap.
The
CC
GC
did
cre
ate
map
s w
hich
m
ust
pres
ent t
he d
ata
with
in a
n co
ncen
trat
ion
map
s do
co
nfid
ence
int
erva
l. C
CG
C
show
the
mag
nitu
de a
nd d
istr
ibut
ion
of th
e st
anda
rd
adeq
uate
con
fiden
ce i
nter
val t
hat
not
incl
ude
any
excl
uded
dat
a fr
om c
onto
ur m
aps
devi
atio
n.
The
sta
ndar
d de
viat
ion
was
use
d to
cre
ate
is ac
cept
able
for
prov
idin
g re
liabl
e in
form
atio
n re
gard
ing
for
wel
ls g
reat
er t
han
400
feet
, in
co
ntou
rs f
or d
iffer
ent c
onfid
ence
leve
ls,
66%
and
95
%.
In
info
rmat
ion
to th
e pu
blic
. ra
nge
of c
onfid
ence
ad
ditio
n to
oth
er re
ason
s.
For
ad
ditio
n, th
e C
CG
C p
rovi
ded
a se
cond
type
of
krig
ing,
indi
cato
r in
terv
al a
nd d
o no
t sta
te
exam
ple,
dat
a w
as a
lso
excl
uded
kr
igin
g, w
hich
pro
vide
s a
prob
abili
ty o
f ex
ceed
ance
at a
ny
that
con
tour
s re
flect
du
e to
ver
y hi
gh c
once
ntra
tions
lo
catio
n in
the
Sal
inas
Val
ley.
pr
edic
ted
nitr
ate
whi
ch C
CG
C s
uspe
cts
are
from
a
We
unde
rsta
nd th
at R
egio
nal B
oard
sta
ff w
ould
like
an
conc
entr
atio
n.
Con
tour
lo
caliz
ed c
onta
min
atio
n si
te o
r ov
erar
chin
g st
atem
ent o
n al
l fig
ures
say
ing
we
excl
uded
som
e m
aps
do n
ot in
dica
te
whe
re d
ata
was
col
lect
ed p
rior
to
wel
ls a
t con
tam
inat
ed s
ites.
O
n th
e co
ntou
r m
aps
we
stat
ed:
whe
n da
ta h
as b
een
the
year
200
0.
Con
tour
map
s "E
xclu
ded
wel
ls i
nclu
de w
ells
with
kno
wn
wel
l dep
th g
reat
er
excl
uded
from
the
indi
cate
dat
a ha
s be
en e
xclu
ded
than
400
feet
or
wel
l use
tha
t is
eith
er ir
rigat
ion
or
inte
rpre
tatio
n.
-
from
the
inte
rpre
tatio
n on
ly
base
d on
dep
th, b
ut d
o no
t id
entif
y da
ta e
xclu
ded
for
othe
r re
ason
s.
Map
s ar
e in
clud
ed th
at d
ispl
ay
stan
dard
dev
iatio
n of
the
nitr
ate
conc
entr
atio
n co
ntou
r map
, es
timat
ed p
roba
bilit
y of
ex
ceed
ing
the
drin
king
wat
er
stan
dard
, an
d di
strib
utio
n of
ni
trat
e co
ncen
trat
ion
at th
e 66
%
and
95%
con
fiden
ce in
terv
als.
C
CG
C c
onsu
ltant
s de
scrib
e th
at
the
66%
and
95%
upp
er b
ound
m
aps
are
prod
uced
by
addi
ng
one
or t
wo
stan
dard
dev
iatio
ns,
resp
ectiv
ely,
to th
e es
timat
ed
conc
entr
atio
ns,
and
that
this
in
dica
tes th
at th
ere
is a
66%
or
95%
con
fiden
ce le
vel
that
the
actu
al c
once
ntra
tion
is b
etw
een
the
uppe
r an
d lo
wer
bou
nd
conc
entr
atio
ns
How
ever
, no
conf
iden
ce i
nter
vals
ar
e pr
ovid
ed r
elat
ive
to th
e
dom
estic
/irrig
atio
n w
ith u
nkno
wn
wel
l dep
th."
In
App
endi
x B
, F
igur
e B
1 st
ates
. "E
xclu
ded
wel
ls in
clud
e w
ells
w
ith k
now
n w
ell d
epth
gre
ater
tha
n 40
0 fe
et o
r wel
l us
e th
at
is e
ither
irrig
atio
n or
dom
estic
/irrig
atio
n w
ith u
nkno
wn
wel
l de
pth,
and
env
ironm
enta
l mon
itorin
g w
ells
in th
e S
alin
as a
rea
with
pos
sibl
e ni
trat
e or
fer
tiliz
er c
onta
min
atio
n."
Act
ually
, as
was
des
crib
ed t
o A
ngel
a S
chro
eter
, for
eve
ry
estim
ated
poi
nt, 1
or 2
sta
ndar
d de
viat
ions
wer
e su
btra
cted
fr
om t
he v
alue
s to
det
erm
ine
the
low
er b
ound
of t
he c
onto
ur
inte
rval
. T
his
proc
ess
was
use
d to
map
the
dis
trib
utio
n of
co
ncen
trat
ions
at t
he 6
6 an
d 95
% c
onfid
ence
leve
ls.
- W
e ar
e un
clea
r wha
t st
aff i
s re
ques
ting
rela
tive
to p
rovi
ding
co
nfid
ence
inte
rval
s fo
r kr
iged
nitr
ate
conc
entr
atio
ns.
Thi
s ca
n be
pro
vide
d on
a po
int b
y po
int b
asis
but
is d
iffic
ult t
o di
spla
y on
a m
ap.
Act
ually
, as
was
des
crib
ed to
Ang
ela
Sch
roet
er, f
or e
very
es
timat
ed p
oint
, 1
or 2
sta
ndar
d de
viat
ions
wer
e su
btra
cted
fr
om t
he v
alue
s to
det
erm
ine
the
low
er b
ound
of t
he c
onto
ur
inte
rval
. T
his
proc
ess
was
use
d to
map
the
dist
ribut
ion
of
conc
entr
atio
ns a
t th
e 66
and
95%
con
fiden
ce le
vels
.
We
are
uncl
ear w
hat
staf
f is
requ
estin
g re
lativ
e to
pro
vidi
ng
conf
iden
ce in
terv
als
for
krig
ed n
itrat
e co
ncen
trat
ions
. T
his
can
be p
rovi
ded
on a
poi
nt b
y po
int b
asis
but
is im
poss
ible
to
disp
lay
on a
map
.
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
, 20
15
Pag
e 12
of 1
4
Item
16
Pub
lic C
omm
ent
2 Ja
nuar
y 29
-30,
201
5 Le
tter
Cen
tral
Coa
st G
roun
dwat
er C
oalit
ion
date
d 1/
26
Con
tour
Map
Crit
eria
Id
entif
ied
in J
uly
11,
2013
C
CG
C W
orkp
lan
App
rova
l,
Sta
ff R
epon
ses
to
CC
GC
Con
tour
M
ap S
ubm
itted
A
pril
30,
2014
Sta
ff R
espo
nses
to
CC
GC
Con
tour
Map
S
ubm
itted
Dec
10
, 20
14
CC
GC
Res
pons
e
krig
ed n
itrat
e co
ncen
trat
ion
cont
our
map
.
Con
ditio
n 11
: C
onto
ur m
aps
shou
ld u
se t
he S
tate
D
rinki
ng W
ater
Sta
ndar
d of
45
mg /L
N
itrat
e as
NO
3 an
d th
e in
itial
co
ntou
r int
erva
ls m
ust
be
appr
oxim
atel
y ev
ery
10 m
g /L
N
itrat
e as
NO
3.
Afte
r re
achi
ng t
he
45 m
g /L
Nitr
ate
as N
O3,
co
ntou
r,
you
may
incr
ease
the
siz
e of
the
co
ntou
r in
terv
al,
if ap
prop
riate
.
Nitr
ate
conc
entr
atio
n co
ntou
r m
ap in
clud
es
appr
opria
te c
onto
ur
inte
rval
s up
to
45 m
g /L
N
itrat
e. A
fter 4
5 m
g/L,
map
onl
y in
dica
tes
45-
390.
5 m
g/L
Thi
s
uppe
rmos
t con
tour
-
inte
rval
doe
s no
t ap
prop
riate
ly id
entif
y ar
eas
abov
e th
e dr
inki
ng w
ater
st
anda
rd, i
nclu
ding
m
axim
um
conc
entr
atio
ns re
port
ed
as h
igh
as 6
90 m
g/L
Nitr
ate
as N
O3.
T
his
lack
of i
nfor
mat
ion
(con
tour
diff
eren
tiatio
n ab
ove
45 m
g/L)
wou
ld
prov
ide
subs
tant
ial
valu
e.
Sam
e co
ncer
ns a
s A
pril
30,
2014
ve
rsio
n. A
fter4
5 m
g /L
Nitr
ate,
m
ap in
dica
tes
a 45
-90
mg/
L an
d
> 9
0 m
g/L
Nitr
ate
rang
e in
conc
entr
atio
n.
The
m
ap d
oes
not
prov
ide
adeq
uate
dat
a an
d
info
rmat
ion
for
conc
entr
atio
ns
rang
ing
from
90
- 690
mg/
L N
itrat
e..
The
inte
ntio
n of
the
CC
GC
was
to p
rovi
de r
eada
ble
map
s fo
r co
ncen
trat
ion
with
mea
ning
ful r
ange
s of
con
cent
ratio
ns
rele
vant
to M
CL.
T
oo m
any
cont
our
inte
rval
s pr
even
t th
e re
ader
fro
m m
akin
g se
nse
of th
e m
ap.
Hyd
roF
ocus
H
ydro
logi
st D
ave
Leig
hton
cor
resp
onde
d w
ith A
ngel
a S
hroe
ter
on t
his
issu
e re
lativ
e th
e P
ajar
o T
echn
ical
M
emor
andu
m a
nd s
he s
tate
d th
at:
"If 1
0 m
g/L
inte
rval
s w
ill.
not w
ork,
ple
ase
let
us k
now
wha
t yo
u re
com
men
d ".
(Ple
ase
see
emai
l tra
nscr
ipt
belo
w.)
We
prov
ided
add
ition
al
cont
our
leve
ls i
n th
e P
ajar
o T
echn
ical
Mem
oran
dum
as
per
Ang
ela'
s re
spon
se a
nd w
ill d
o so
for
the
Sal
inas
Val
ley
in th
e C
hara
cter
izat
ion
Rep
ort.
Con
ditio
n 12
: T
he s
ampl
ing
dens
ity,
reso
lutio
n an
d sc
ale
mus
t be
ap
prov
ed b
y th
e E
xecu
tive
Offi
cer,
in
adva
nce
of
cont
our
map
pre
para
tion,
to a
void
th
e pr
oble
m o
f not
hav
ing
suffi
cien
t da
ta t
o pr
oduc
e an
acce
ptab
le c
onto
ur m
ap.
CC
GC
did
not
pro
vide
sp
ecifi
c in
form
atio
n re
gard
ing
sam
plin
g de
nsity
, re
solu
tion,
and
scal
e to
the
Exe
cutiv
e
Offi
cer
in a
dvan
ce o
f the
su
bmitt
al o
f th
e co
ntou
r m
ap,
and
so n
one
was
appr
oved
.
CC
GC
did
not
pro
vide
spe
cific
in
form
atio
n re
gard
ing
sam
plin
g
dens
ity,
reso
lutio
n, a
nd s
cale
to
the
Exe
cutiv
e O
ffice
r in
adva
nce
of t
he s
ubm
ittal
of t
he c
onto
ur
map
, an
d so
non
e w
as a
ppro
ved.
The
CC
GC
info
rmed
the
Reg
iona
l Wat
er B
oard
tha
t the
CC
GC
wou
ld u
se e
very
dom
estic
wel
l ava
ilabl
e.
As
disc
usse
d ab
ove,
we
coul
d no
t, no
r ca
n R
egio
nal
Boa
rd s
taff,
iden
tify
addi
tiona
l do
mes
tic w
ells
to b
e sa
mpl
ed.
-
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
, 20
15
Pag
e 13
of
14
Item
16
Pub
lic C
omm
ent
2 Ja
nuar
y 29
-30,
201
5 Le
tter
Cen
tral
Coa
st G
roun
dwat
er C
oalit
ion
date
d 1/
26
Con
tour
Map
Crit
eria
Id
entif
ied
in Ju
ly 1
1, 2
013
CC
GC
Wor
kpla
n A
ppro
val
Sta
ff R
epon
ses
to
CC
GC
Con
tour
M
ap S
ubm
itted
A
pril
30,
2014
Sta
ff R
espo
nses
to
CC
GC
Con
tour
Map
S
ubm
itted
Dec
10
, 20
14
CC
GC
Res
pons
e
Con
ditio
n 12
:
Con
tour
map
s fo
r the
co
oper
ativ
e pr
ogra
m m
ust
be
deve
lope
d by
, or
und
er t
he
revi
ew o
f a r
egis
tere
d P
rofe
ssio
nal G
eolo
gist
or
Pro
fess
iona
l Eng
inee
r
Con
tour
map
s w
ere
prep
ared
by
Ste
ven
Dev
erel
, a re
gist
ered
P
rofe
ssio
nal
Geo
logi
st in
the
Sta
te o
f C
alifo
rnia
.
Con
tour
map
s w
ere
prep
ared
by
Ste
ven
Dev
erel
, a
regi
ster
ed
Pro
fess
iona
l Geo
logi
st in
the
S
tate
of C
alifo
rnia
.
Ste
ven
Dev
erel
a P
rofe
ssio
nal G
eolo
gist
dev
elop
ed t
he c
onto
ur
map
s..
Con
ditio
n 12
:
Con
tour
map
s m
ust b
e ba
sed
on a
sam
plin
g de
sign
that
is s
tatis
tical
ly
defe
nsib
le g
iven
the
spat
ial
varia
bilit
y of
the
aqu
ifer
(i.e.
, hy
drog
eolo
gica
l he
tero
gene
ity,
etc.
) an
d sp
ecifi
c lo
cal c
ondi
tions
.
Con
tour
map
s ar
e ba
sed
on C
CG
C
sam
plin
g an
d av
aila
ble
data
, w
ith s
ome
data
excl
uded
. T
here
is n
o
disc
ussi
on t
o ev
alua
te
whe
ther
the
data
is
suffi
cien
t gi
ven
the
spat
ial
varia
bilit
y of
the
aqui
fer a
nd s
peci
fic
loca
l con
ditio
ns.
Sam
e as
Apr
il 30
, 20
14,
vers
ion.
R
evis
ed T
ech
Mem
o do
es
incl
ude
disc
ussi
on re
late
d to
st
anda
rd d
evia
tion.
The
Tec
hnic
al M
emor
andu
m s
how
s go
od a
gree
men
t with
m
easu
red
and
sim
ulat
ed v
alue
s at
loc
al s
cale
s. T
he
stan
dard
dev
iatio
n va
lues
are
dis
cuss
ed o
n pa
ges
43 a
nd 5
3.
Con
ditio
n 12
:
Con
tour
map
s m
ust
be p
rovi
ded
as
a ge
ogra
phic
info
rmat
ion
syst
ems
(GIS
) sh
apef
ile a
ccor
ding
to
a
spec
ific
time
sche
dule
.
CC
GC
pro
vide
d G
IS f
iles
to t
he W
ater
Boa
rd.
GIS
file
s no
t pr
ovid
ed a
t tim
e th
e S
taff
Rep
ort w
as w
ritte
n.
File
s w
ill b
e pr
ovid
ed a
t th
e tim
e of
the
subm
issi
on o
f the
ch
arac
teriz
atio
n re
port
.
Con
ditio
n 13
:
Con
tour
map
s m
ust c
lear
ly
desc
ribe
the
met
hod
used
to
cont
our t
he g
roun
dwat
er
mon
itorin
g da
ta,
the
asso
ciat
ed
conf
iden
ce in
terv
als
and
the
area
s
of u
ncer
tain
ty.
Con
tour
met
hod
used
is
krig
ing.
C
onfid
ence
in
terv
als
are
not
incl
uded
on
the
map
or
in th
e re
port
. A
reas
of
-
unce
rtai
nty
are
not
repr
esen
ted
on c
onto
ur
map
.
Krig
ed n
itrat
e co
ncen
trat
ion
map
s ar
e id
entif
ied
as e
stim
ated
va
lues
, but
do
not
incl
ude
any
info
rmat
ion
rega
rdin
g ra
nge
of
conf
iden
ce i
nter
val.
See
di
scus
sion
abo
ve.
Thi
s is
an
inco
rrec
t sta
tem
ent a
s m
aps
with
var
ying
co
nfid
ence
lev
els
are
prov
ided
and
exp
lana
tions
of t
hose
in
terv
als
are
also
pro
vide
d. (
see
Fig
ures
20
and
21)
CC
GC
Res
pons
e to
Sta
ff R
epor
t Ja
nuar
y 26
, 20
15
Pag
e 14
of
14
Item
16
Pub
lic C
omm
ent
2 Ja
nuar
y 29
-30,
201
5 Le
tter
Cen
tral
Coa
st G
roun
dwat
er C
oalit
ion
date
d 1/
26
ATTACHMENT 8
1/27/2015
Centrat Coast Groundwater Coa[itfon
Central Coast Regional Board Meeting
January 30, 2015
Parry Klassen
Executive Director
Membership Status
iiL
Category Count Percentage
Total Number of Members 578
Total Acreage 201,572.69
Sum of Acreage - North 137,560.87 68%
Sum of Acreage - South 64,011.82 32%
7, 1, 7 7
Item 16 Presentation 2
January 29-30, 2015 CCGC
ATTACHMENT 8
1
Sampling and Exceedance Statistics Groundwater Sub Basin
Total Well Counts
Pot Domestic Wells
o of Domestic Exceedances Exceedances
SALINAS VALLEY 249 235 118 50% GILROY-HOLLISTER VALLEY 145 141 34 24%
PAIARO VALLEY 85 74 23 31%
LOCKWOOD VALLEY 2 2 0
SANTA CLARA VALLEY - SANTA CLARA 5 5 2 40%
SANTA CRUZ PURISIMA FORMATION 5 5
TRES PINOS VALLEY 1 1 o
SANTA MARIA 309 74 49 58%
SANTA YNEZ RIVER VALLEY 138 55 1 2%
SAN LUIS OBISPO VALLEY 6 3 2 67%
CARPINTERIA 17 3 0
LOS OSOS VALLEY 12 5
SAN ANTONIO CREEK VALLEY 32 11 0 CUYAAAA VAUE Y 10 4 1 25%
MORRO VALLEY 9 6 0 MONTECITO 1 0 SANTA ANA VALL EY 1 1 1 100%
I
CHOLAME VALLEY 1 1 0 CHORRO VALLEY 1 0 0
Outside Bean Boundary 77 46 2 4%
TOTALS 1106 672 229 34",
Replacement Water Follow Up Statistics
Replacement Water Action Grand Total
Bottled Water 123 Bottled Water/Filtration System i Bottled Water/Ion Exchange 3
Bottled Water/RO Unit 3
Filter i Not Used 41
RO Unit 83 Pending Response 6 Replacement Water Refused by User 4 None Supplied 7
Grand Total 272
1/27/2015
Item 16 Presentation 2
January 29-30, 2015 CCGC
2
1/27/2015
First Technical Memo for Salinas Valley submitted April 2014
Initial contouring
Intention was to share results with Regional Board and receive feedback
t 838 wells used
Kriging analysis used a method that resulted in conservative estimates of where nitrate concentrations are over the MCL.
Resulted in large uncertainty where there were not samples or where the spatial variability was large.
E T WOE SUBAREA
Map showing distribution' of standard deviation
Hotter colors indicate higher uncertainty
CORRAL DE TIERRA AREA
PRESSURE SUBAREA . tiL..:..
. =.4".9; ` . .3¡ 'FOREBAYSVBA l,4.: ..!.
-.3, Jh_f
,a
EXPLANATION Standard Error vwa..d ar m.pprp
C 0.1.10 O Groundwater Bash
L_s:4 J 1020 P._3 20 . 30
MI JO 40
'UPPER VALLEY SUB
3
Item 16 Presentation 2
January 29 -30, 2015 CCGC
1/2.7/2015
xaortionat welts ror December Technical Memorandum
, /' . FOREBAY SUBARG 1 j ,.a >+s .- = D t; +' b.. 44'.
- ,,7," , ' .
yyss .: ".rOPPBR VALLlV
EXPLANATION Standard Error - weas mu, brn.00bti
O t r0 Rawnbl.wmpMUC000 weY 10 .20 RaunMreaNMONOIwelly
0raa4rnkBoyle >v.0
116111', Erin s0eo i.tl.M...
I
lRIru.ea.e...oara .....1101.40.0111 . A4.,aRal.rada..BIFO.. ...,,
u ']tM .
I t A ) kI.P
EXPLANATION -- \t..1 Nltra;a Dab
IQQW/110Jn iSlkl Lam PAlnd 01 OM CORSfiS11C.Irdrrsl
®
tTb M../.l d C(OC 1aRY rats .9 9.9.99O ia)rOSK nra.r<tanaa::ena.a..BA.OL+I OQ.iRlrvsApQ»1fFa.tlhaO.Si.u.ln I
.Oral crklb wpb saY.dMOax ..... ar btLi-WdSgI! arayr La WL ...
Number of Wells Used in Analysis: 939
Type of Kriging Analysis Used: maximum nitrate values from wells with multiple values, Ordinary Kriging using logarithms of the concentrations provided greater agreement and lower and standard deviation.
Comparison maps provided in Appendices
4
Item 16 Presentation 2
January 2.9 -30, 2015 CCGC
1/27/2015
... ..
-..n."
.t.
.,...
-..
` ' .
. ., ..
yyy
_
'.,; 'It
r - '
,
,
}...eJ Ì
g
ti. e
.. .
. i" SEASIDE
AREA _ y y: m
CORRAL DE
! TIERRA AREA -`1, \ V.
_.. ._ _-.
M>.isWeabtNab<iOrOVe Vann Ereera.avet ravx..tr web bwrervahe.I<rk.tt.n.00a.ta NkRrtaU.dterkabtbLlel/?ptaavo m.sAmaron
" I i d -.S
` ; ' .. . ,,.. .I `,
.._ .
L ~
; .
e {í'
.r
.. _
- EXPLANATION - _- - y..g. eAR NO] Data
Ek.netlgNO3Ca.aM+.nw
TIS C124 76 Da-U u-p ' Driaedge4r8efbl
a ® a
.- dVt.Weaedbrea.r.uapFyr.Mm..taOA...'il .be...a.tiawr..raee.ltryMHer400ba .qa.lYtbnrMerJe. av«kaepse.a.
illr va,wrn..eahn
_e. ' IANOLEyAREA
r
- - " ! :j - n .., - . ,
.1.. D.
,
:,
b
,
r C t
a `\ . . EASTSIDESUBAREA
ó
\,,.: ' / ' e
\ t ' . .
' 'ï r = f `
" / PRESSURE i -
SUBAREA r - a
.- i: I.
"4.';:"-):,'' .) .i `
.. -
Ir
,
^ UPPER V. A:. LLEY SUBAREA
, ,,', .... r,.
.--
.
,
EXPLANATION Nböe mN NO3 Deb
FsbntbNOJGewereóee0a . t (012_3 34
1=131143 sou. m' DffpeAe/MrBatia
e i
.-..._
Ito bakesaÌCOOCr.xaröaK-.talg..lMabea sytl03MakOaF.ekrM.siamnem.aR. .ary b pO.q r..a.: e.,.ay TM.ka w petal Or a t ri .bá.kanaa.ra.w,,aa..¢
51^ zó(.F.w?ät.wywSfi+.dGe
Rbe.eaaktxacr.nber.eb.tteranaoa/y.a. a) b03 man hoan e. p+W a mroAi Oecemt b pdeet inxaa.t pl.sea Tb aM a pMM.K. t M eana.mawrn.rtkeeboVn
a;.._ a.. w,.. :n+a
r ... .. i.. ,..« ...-. ....
600
Comparison of map- estimated nitrate concentrations versus measured nitrate concentrations
y = 0.9819x - 0.0548, ----
5
Item 16 Presentation 2
January 29 -30, 2015 CCGC