|Reference : Representing Grassed Buffer Strips’ Hydrology in a Regional Scale Model|
|Scientific congresses and symposiums : Unpublished conference/Abstract|
|Life sciences : Environmental sciences & ecology|
|Representing Grassed Buffer Strips’ Hydrology in a Regional Scale Model|
|Sohier, Catherine [Université de Liège - ULg > > Gembloux Agro-Bio Tech >]|
|Degre, Aurore [Université de Liège - ULg > > Gembloux Agro-Bio Tech >]|
|Riparian buffer strips as a multifunctional management tool in agricultural landscapes : workshop of the cost action 869|
|25-28th april 2010|
|Macaulay land use resarch institute|
|[en] buffer strip ; hydrology ; regional modelling|
|[en] In Walloon Region (Belgium), like in many other European countries, riparian buffer
strips appear to become one of the most approved nutrient mitigation measures.
Within the frame of the water framework directive, policy makers need nutrient
mitigation forecasting at the scale of the surface water bodies (from 3 to 426 km² in
Wallonia). It induces that the hydrological models have to deal with different designs
of the buffers themselves and of their catchment areas.
Up to date, most of the studies focused on sediment deposition at field scale. They
concluded that the grassed strips can be very effective; nevertheless, the measured
effects are still very variable. More often, the way the runoff water passed through the
buffer strip (diffused or concentrated flow) is not considered.
We adapted our regional hydrological model (physically based, spatially distributed
over the 17.000 km² Walloon region (Sohier et al., 2009)) by developing a new “buffer
strip subroutine” that identifies automatically the catchment area of all the buffer
strips. This is done using a 10 m resolution DTM. The catchment area is then
subdivided into an “area of flow concentration” that leads the water to pass through
the buffer strip on a very small portion of it and into an “area of diffuse flow” that leads
the water to pass through the buffer strip using its whole length. The daily fluxes of
water, nutrient and sediments that pass through the buffer are calculated by the
model using our dynamic geodatabases (soil, DTM, weather, land use, agricultural
practices). Depending on whether the flow is diffused or concentrated the water
depth can vary to a large extent; so does the deposition ratio (algorithm adapted from
The buffer itself is modelled as grassland without direct fertilisation. Water and
nutrient coming from the watershed can be used by the grass, water can infiltrate,
evaporate or runoff and denitrification can occur when the soil is saturated.
The oral presentation will show our results at the water body level for different buffer
strip scenarios considering sediments and nitrate reduction in surface water.
|COST action 869|
|Researchers ; Professionals ; Students|
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