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Land use effect on nutrient loading – nutrient models new assessment tools Inese Huttunen, Markus Huttunen and Bertel Vehviläinen Finnish Environment Institute
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Basic structure of WSFS-Vemala Hydrological WSFS-model: Inputs daily precipitation and temperature Simulates hydrological cycle on daily time step Covers all Finland, 6200 sub-basins, 58 000 lakes Simulated daily Data-assimilation, ensemble forecasts Water quality simulation with Vemala Diffuse loading (agriculture and non-agriculture) Point load, settlements, atmospheric deposition Simulates transport in rivers and lakes Total phosphorus, total nitrogen, suspended solids, organic carbon (TOC)
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Relationship between concentration and runoff / use of VIHMA annual loads Runoff r (= r1+r2+r3+r4+r5) is divided into 5 classes r x, each class has Ptot concentration c x,x which is calibrated r1: runoff in runoff class 1, 0-1 mm/day r2 runoff in runoff class 2, 1-3 mm/day r3 runoff in runoff class 3, 3-6 mm/day r4 runoff in runoff class 4, 6-10 mm/day r5 runoff (unlimited) in runoff class 5, > 10 mm/day Concentration relationship with runoff VIHMA tool (Puustinen, SYKE) is used to simulate annual agricultural load and Vemala load is adjust 1 100 000 field plots are simulated separately by knowing slope, plant, soil type, P soil
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Nutrient balance in lakes Inflow loading Outflowing load Sedimentation Internal load Accumulation = Loading – outflow – sedimentation + internal loading Annual Phosphorus balance for Karhijärvi Inflow loading 10.2 t Outflow load 8.9 t Sedimentation 5.9 t Internal loading 3.2 t
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Calibration Calibration is the process of modifying the parameters to a model until the difference between output from the model and observed data sets is minimum Optimization criteria is: all observation points located at the same calibration area are taken into calibration: + there is a need to use all available observations in the calibration even if the are very infrequent (few times per year), − more frequently observed points gets more weight in the calibration procedure. appropriate weights for each type of observations are found and tested to reach the best possible calibration result Water quality observations are not daily
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Phosphorus concentration
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Phosphorus load
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Agricultural load 59% of the total loading into Archipelago Sea
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Use of VEMALA to simulate different scenarios Vemala can be used to simulated present situation We can change present loadings and simulate concentrations and loadings in the river catchments in changed conditions: Possible changes are: Crop management changes by VIHMA / ICECREAM Wetland effect Scattered settlement loading changes Point load changes Climate change scenarios Combination of above mentioned Scenario simulations has been done in TEHO project for Aurajoki, Loimijoki and Eurajoki
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Wetland simulation All possible small ditch catchments with area 20 – 200 ha Which has at least 20% of agricultural fields Its possible to simulate the effect of all possible wetlands, we can simulate nutrient sedimentaion in wetland, plant uptake
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Scenarios of agricultural practices in TEHO Buffer zones Increase of vegetation cover during the winter (30%, 50%, 70% of the total agricultural area): Equally in all catchment On the steeper sloped fields Using of mannure decreased by 50% Decresed using of P fertilizer Conclusions from TEHO scenarios: There is no one single method to reduce agricultural loading, seceral reduction methods need to be combined The best reduction can be achieved by combination of: Increased vegetation cover on fields over 3% slope Buffer zones are established Reduced P fertilizer application, that P soil < 14 mg/l Best management practices of mannure apllication
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Summary Agricultural load needs to be reduced to improve the state of the Baltic Sea Mitigation measures are done on the field scale and there are needed tools to estimate what is the effect of mitigation measures on the river catchment scale Nutrient load models (Vemala) can be used to simulate different scenarios how should the agricultural practices be changed to reduce the agricultural loading There are no one single method to reduce agricultural loading, its a combination of methods More detailed process description improves the models capability to simulate climate change or agricultural management scenarios
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Thank You! www.environment.fi/waterforecast
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