tóth et al
TRANSCRIPT
Spatial distribution of halobity in floodplain related to OM
accumulation
Gabriella Tóth, Amadé Halász, József Dezső, Jakub Miřijovský, Dénes Lóczy
Hungarian Scientific Research Fund
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Old-Drava Rehabilitation Programme (ODP) ”ecologically sustainable and cost-effective water supply”
Research area of Univ Pécs (2013-14)
Cún-Szaporca oxbow
„check the ODP plans”
planned pipe or channels
for water recharge and
regulation
lakes, oxbows under
revitalization
settlements
planned reservoirs
forests with
planned irrigation
arable with
planned irrigation
sluices
The planners* set the following criteria for the regulation of water level: • Water level fluctuation should not exceed 0.5 m within a year; • Water recharge should take place step by step, in divisions; • In a year water recharge should be implemented by not more than two
fillings; • The length of the filling period should remain within two weeks.
*In the planning document Old Drava Project
Problematic planning concept and calculations
• Success of water recharge is questionable: hydraulic connection not clear
• Quality of inflow water is different from that in the oxbow
• water quality parameters of Lake Kisinc are not pecisely known
Study area
• Area: 20 ha
• Length: 2 km
• Average latitude: 100 m
• Average depth: 1 m
•Lake Kisinc, one of the remains of the late Old- Drava bed •The bank is significantly covered with tangle
Problems
• Lack of water, water quality,
• Exploitation of the lake, aims (by planners):
• Protection of ecologycal/natural values, restitution of wetlands;
• ‘Establishment of sustainable water-management in the region’
• ‘Development of tourism and recreation’
Water quality of Fekete-víz stream EC: 937 μS; DO: 5.72 mg/l; O2: 68.8%, KOI: 8.7 mg/l
Feeder canal
(under construction)
Water quality of Drava river (earlier natural water supplier, until 1976) EC: 283 μS; DO: 8.99 mg/l; O2: 101.1%, KOI: 4.1 mg/l
The aim
• Measure Lake Kisinc (oxbow), waterchemistry, the daily dynamism of the parameters (halobity)
• Is the condition suitable after a cool and rainy summer, by the measured parameters?
Mesotrophic condition Eutrophic condition
Phosphorous
µg/l 10-30
Phosphorous
µg/l 30-100
Total
nitrogen µg/l 400-600 Total
nitrogen µg/l 600-1500
Measurements
In field: Rapidly varying parameters: WTW 390i pH C° Redoxpotential Soluted O (mg/l, (%)
In laboratory: Nanocolor 500D VIS NH4
+, NO3- -- PO4 PO4-T KOI
2 4 6 8 10 12 14 16 18 20 22 241819202122237,0
7,2
7,4
7,6600
650
700
7501
2
3
410
20
30
40
5020
30
40
0,060,080,100,120,14
0,10
0,15
0,200,0
0,1
0,2
0,3
0,40
1
2
3
2 4 6 8 10 12 14 16 18 20 22 24
16
18
20
22
hours (210cm)
T(water) (°C)
pH
EC (µS)
O2 (mg/l)
O2 (%)
KOI (mg/l)
Orto-P (mg/l)
Total-P (mg/l)
nitrate (mg/l)
ammonium (mg/l)
T (air) (°C)
2 4 6 8 10 12 14 16 18 20 22 24
20
21
22
7,6
7,8
8,0540545550555560565
2
3
4
5102030405060
24
26
28
300,00
0,04
0,08
0,06
0,08
0,10
0,120,02
0,04
0,06
0,080,00,10,20,30,4
2 4 6 8 10 12 14 16 18 20 22 24
16
18
20
22
hours (30cm)
30cm
30
EC (µS)
O2 (mg/l)
O2 (%)
KOI (mg/l)
Orto-P (mg/l)
Total-P (mg/l)
nitrate (mg/l)
ammonium (mg/l)
T (air) (°C)
Results • No thermo-stratification
Oxygen:
ORP: -210 cm (kb – 30 mV)
O2: low (mg/l) also in saturation %
C circulation:
KOI: high
Phosphorous forms:
Orto- and total phosphate grate – adequate
Nitrogen forms:
nitrate, ammonium: great - tolerable
Conclusion 1. Bad water quality remains
2. Shallow depth: deeper layers (-210cm) heat up, low soluted O2 capacity
3. ORP: deeper layers are reductive (average: -30mV), high KOI: high organic matter content
4. Moderated transport of nutrients
5. The bigger water surface won’t owe adequate depth
6. Periodically refilling from Dráva river (I. class water quality): inland inundation