factors contributing to the internal loading of phosphorus from anoxic sediments in six maine (usa)...
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FACTORS CONTRIBUTING TO THE INTERNAL LOADING OF
PHOSPHORUS FROM ANOXIC SEDIMENTS IN
SIX MAINE (USA) LAKES
Bjorn LakeDoctoral Student
Civil and Environmental EngineeringThe University of Maine
Research Goals
• Perform a sedimentary analysis on six lakes with varying trophic status using a common sequential extraction procedure.– Delineate P, Al, and Fe speciation in the
sediments– Decipher any temporal trends in sediment P, Al,
and Fe speciation– Determine any correlations/predictors that are
characteristic of lakes with internal P load
• Calculate sedimentary P-flux using publicly available water column data and bathymetric data from Maine DEP
Background
• How do lakes become anoxic?• What controls phosphorus availability?
• Why is phosphorus important?
Al(OH)X
Classic Model of P Sorption
Fe Fe 3+3+
Ferric ionFerric ion
Fe Fe 2+2+
Ferrous ionFerrous ion
Fe(OH)Fe(OH)XX
Iron HydroxideIron Hydroxide
SRPSRP
SRPSRP
Anoxic
Oxic
Study Lakes
• Highland Lake • Pennesseewassee
Lake• Salmon Pond• China Lake• Webber Pond• Cobbosseecontee
Lake
Hydrologic Characteristics
High P/ Low P
Max Depth
Mean Depth
Surface Area
Drainage Area/ Surface
Area
Flushing Rate
Perennial Inlets
Intermittent Inlets
m m ha yr-1China H 25.9 8.5 908 19.3 0.72 6 54Cobb H 30.5 11.3 2120 10.2 1.07 8 2High L 20.0 6.0 252 10.2 0.91 6 2Penn L 14.6 5.5 384 31.3 1.38 9 1Salm H 17.4 7.0 270 7.8 0.54 2 26Webb H 12.5 5.5 485 11.2 1.52 4 15
Lake
Sequential ExtractionSedimentSediment
ResidueResidue
ResidueResidue
ResidueResidue
Ca-PCa-PLabileLabile
NaOH-TPNaOH-TP NaOH-rPNaOH-rP NaOH-nrPNaOH-nrP- =
1 M NH4Cl @ pH 7
1 M NaOH
0.1 M Na2S2O4/NaHCO3
0.5 M HCl
1 M NaOHFe-PFe-PResidueResidue
ResidueResidue Refractory-PRefractory-P
Al-P Org./Bact.-P
Digestion
Extraction Results0 10 20 30 40 50 60 70
Hig
hlan
d
MayJulySept
Pen
n MayJulySept
Sal
mon May
JulySept
0 50 100 150 200 250
Chi
na
MayJulySept
Ext-P mol g-1
0 50 100 150 200 250
Cob
b MayJulySept
0 10 20 30 40 50 60 70
Web
ber
MayJulySept
NH4Cl-P
BD-P NaOH25-P
HCl-P NaOH85-P
0 100 200 300 400 500
Hig
hlan
d
MayJulySept
Pen
n MayJulySept
Sal
mon May
JulySept
0 200 400 600 800 1000
Chi
na
MayJulySept
Ext-Fe mol g-1
0 200 400 600 800 1000
Cob
b MayJulySept
0 100 200 300 400 500
Web
ber
MayJulySept
NH4Cl-Fe
BD-Fe NaOH25-Fe
HCl-Fe NaOH85-Fe
0 5 10 15 20 200 400 600 800 1000
Hig
hlan
d MayJulySept
Pen
n MayJulySeptS
alm
on MayJulySept
Chi
na
MayJulySept
Cob
b MayJulySept
Ext-Al mol g-1
0 5 10 15 20 200 400 600 800 1000
Web
ber May
JulySept
NH4Cl-Al
BD-Al NaOH25-Al
HCl-Al NaOH85-Al
Prerequisite 1
NaOH25-Al:[NH4Cl-Fe+BD-Fe]
0 1 2 3 4 5 6
SR
P [
NH
4C
l-P+
BD
-Fe]
0
20
40
60
80
100
HighlandPenneesseewasseeSalmonChinaCobbosseeconteeWebber
Prerequisite 2
March May July September November
NaO
H2
5-A
l:[N
H4C
l-P+
BD
-P]
25
75
125
300Highland Penneesseewassee Salmon China Cobbosseecontee Webber
Calculated P-Flux
Webb (11) Salm (8) China (15) Cobb (16) Penn (7) High (15)
P F
lux
(mg
m-2
d-1
)
0
2
4
6
8
Al:Fe vs. P Flux
NaOH25-Al:[NH4Cl-Fe+BD-Fe]
0 1 2 3 4 5 6
P F
lux
(mg
m-2
d-1
)
0
1
2
3
4
5
Cobbosseecontee
Webber
China
Salmon
Highland
Penneesseewassee
Conclusions
• Prerequisites for low P release NaOH-Al:[NH4Cl-Fe+BD-Fe] > 3* NaOH-Al:[NH4Cl-P+BD-P] > 25* [NH4Cl-P+BD-P]:TP < 0.1
• Other possible factors Alkalinity during summer Fe-flux during summer †
Quality of organic matter
* Kopačék et al. (2005)† Amirbahman et al. (2003)
Alkalinity
Webber
Salmon
China
PennHighCobb
0
2
4
6
8
10
12
14
16
0 50 100 150 200 250 300
Alkalinity
P F
lux
* Pearce (1999)
Fe-flux
Future Research
• What’s going on in Cobbosseecontee?
• What role does Org-P have in anoxic sedimentary P-flux?
• How accurate is water column data for calculating P-flux?
AcknowledgementsAcknowledgements
• Kyle CoolidgeKyle Coolidge• Advisory CommitteeAdvisory Committee
• Maine DEPMaine DEP• Environmental Chemistry LaboratoryEnvironmental Chemistry Laboratory
• National Science FoundationNational Science Foundation• NEAEBNEAEB
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