outline loading –concentrations littoral-open water interactions cyanobacteria and nutrients, n:p...
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Outline
• Loading –concentrations• littoral-open water interactions• cyanobacteria and nutrients , N:P• nitrogen-macrophytes• temperature cyanobacteria• diffuse loading problem
• focus on Lake Taihu…
Plake= Pin/(1+tw), tw = y-1
After 10 years
Chen et al, 2003
P-lake/P-in*100
Hydraulic retention time (years
P-lake=P-in/(1+retention time**0.5)
Lake Taihu retetention estimated:39% - ”measured”35% (Qin, 2007)
Zhu et al, 2006
Bioavailable P
Bioavailable P typically >500-2000 in DK lakes
Lake Arresø
Area 40 km2
% of country area 0.09
Mean depth 3.1 m
Max depth 5.9m
Tw 3.5 y
Lake Taihu
Area 2338 km2
% of country area0.02!!!
Mean depth 1.9 m
Max depth 4.5m
tw 0.8 y
Hydraulic retention time:3.5 years
Simple dilutionThree retention times (10.5 years) reduced by 95%
Jeppesen et al ,2007
Jeppesen et al ,2007
Resuspenion does not prevent improvements-even in relatively large shallow lakes
Fraction of suspended solidsmade up by detritus and inorganic SS
Seasonal phosphorus concentrations (relative to winter values) in 265 shallow Danish lakes with different P levels.
Seasonal changes in P concentration
Seasonal P concentration and retention in 14 shallow Danish lakes with reduced P
Phosphorus release mechanisms/factors
•Physical: temperature• Chemical• Biological
Thickness of oxidised surface layer in four lakes at 7, 14 and 21 oC
Cumulative P release from four lakes at 7, 14 and 21 oC.Based on Jensen et al. (1992)
• P release increases at rising temperatures due to increased mineralization and oxygen/nitrate consumption, thus diminishing the oxidised surface layer.
Temporal variation in P
Model
dPV/dt = (Q/V)*[Pin]-SED+REL waterdPS/dt = SED-REL-IMM sediment
SED = bS*PV/ZREL = bF*(tF^(TEMPV-20))*PSIMM = bI*PS
parameters from the Danish model: bS=0.0695, bF=0.000468, tF=0.0867, bI=0.0000923. - 16 lakes-many years
PV og PS [g/m^2], rates [g/m^2/d].
Time step 1 month
TP (mg P l 1)
0.00.10.20.30.4
Time (days)
0 720 1440 2160 2880
TP (mg P l 1)
0.00.51.01.52.02.5
Time (days)
0 720 1440 2160 2880Borup
Examples of the seasonal P-model
Useful for Lake Taihu?Maybe if including the hydrodynamics
Lake Engelsholm
Before fish removal: 1989-1993
After fish removal : 1994-1999
Søndergaard et al,2003
P dynamics
Simple models useful?
Complex models taking hydrodynamicsinto account better?
Sediment –water interactions – how to do realistic experiments
Spatial and temporal variability
Role of N for P release, role of macrophytes (bays), role of fish
What happens when N is passing through a lake
log (NTOT) =
-0.80±0.08 +0.82±0.03 log (TNOTin) +0.13±0.03 log (Z) -0.20±0.02 log (TW) r2 = 0.75
log (NO) = -2.17±0.08 +0.95±0.03 log (NOin) +0.53±0.04 log (Z) -0.43±0.02 log(TW) r2 = 0.92
lake intercept inlet mean depth retention time
Lake Taihu: 1.9 m mean depth, 5month retention time
prediction 56% loss - ”measured” 49%
N-lakerelated to:-Depth-TW-N-in-Temp
Loading
Retention
Retention (%)
Transformations within the nitrogen cycle in shallow aquatic systems(Slide modified from version of Soonmo An)
PONNO3
-
NO2-
NH4+
DON
N2
N2O
PON
DON
NO3-
NO2-
NH4+
N2
N2ONO3-
Sinking
DENITRIFICATION
Fixation
Assimilation
Excretion
Sediment
Water column
DNRA
N-dynamics (chemical perspective)
Mark in Actionat Lake TaihuChina
McCarthy et al,2007
McCarthy et al,2007
N dynamicsSimple models useful?
Complex models taking hydrodynamicsinto account better?
Sediment –water interactions – how to do realistic experiments
Spatial and temporal variability
Role of macrophytes (bays), role of fish
Lake water changes during 10 days at changing wind speed (from 0-2 to 5-7 m/s to 2-3 m/s) in Western Stadil Fjord, Denmark (450 ha, mean depth: 0.8 m).
•Physical: resuspension by wind/benthivorous fish
•Resuspension increases turbidity and sediment-water interactions, particularly in very shallow lakes.
•Submerged macrophytes and floating leaved plants may put a damper on the impact of resuspension. (Huang et al,2007)
Pelagic- littoral zone interaction , Bay-main lake interactions
Huang et al, 2007 - resuspension 50% of open water in Trapa beds.
Wang ,2007 - Higher concentration of nitrate in the reedzone than 200 m away – indicating that trapped nutrients are released from in here and trabsported to theopen water.
Littoral-open water interactions (trap-release) an important research area . Redsistribution of sediment as well.
Local removal of sediment a relastic symptom treatment?
Diatoms
Silicate
Cyanobacteria
green algae
Lake ArresøJeppesen et al ,2007
Chen et al,2003
Water clarity increases not leastafter zooplanktonbiomass and body size increases
Shallow Danish lakes
N-fixing Cyanothennon-N fixing Cyanothen Green algae
with increasing TP
Jensen et al, 1994
N fixers at intermediate TN:TPnot low TN:TP
Green algae and not N fixingcyanoes at the lowestinorganic N
Jensen et al, 1994
Søndergaard et al, 2005
Deep
Shallow
Deep
High N input-- Enhances or reduces importance of cyanobacteria?
or is P affinity the important factor ?
is N:P at all of importane in shallow lakes?
Should we focus on nutrient release /turnover insteadand on benthic pelagic coupling
Changes in water temperature in Danish survey lakes 1989-2005
simpel lineær regression
Model: log(cyanobacteria biomass) = log(TP), log (mean depth), log(wat. temp.)
Jeppesen et al, in prep.
Model: log(cyanobacteria biomass) = log(TP), log (mean depth), log(wat. temp.)
Jeppesen et al, in prep.
Climate warming will likely enhance the risk of cyanobacteria dominance and the duration of blooming during the year
Gonzales Sagrario et al, FWB , 2005
Biomass submerged plants
last day
one with plants
Perihyton and phytoplankton growth stimulated by N thereby out-shading the submerged macrophytes
N threshold not a constant!!!various with fish density and probably climate
Comparative studies
Uruguay (30°-35°S)
Denmark (55°-57°N)
Meerhoff et al, in press,submittedand on the road
Littoral communities structure
High N may lead to losses of macrophytes in temperate lakesat intermediate high TP
How about Lake Taihu plant communities?
Warmer winters than in DK , much warmer summers
Role of fish different or?.
A challange with diffuse loading!!!
Nett accumulation of phosphorus in Danish agriculture
(Dalgaard & Kyllingsbæk, 2003)
TN and TP in Danish lakes
Søndergaard et al, in press
Søndergaard et al, in press
Shallow
all seasons, but see spring May, June ,autumn
TP TN
Slope for log chla = x log TP + y log TN
month
TP
TN
FLORIDA - DENMARK
month
X Y
Weyhenmeier et al, in press