4.6 Article

Simulated event-scale flow and sediment generation responses to agricultural land cover change in lowland UK catchments

Journal

HYDROLOGICAL PROCESSES
Volume 36, Issue 2, Pages -

Publisher

WILEY
DOI: 10.1002/hyp.14474

Keywords

agricultural land cover; catchment modelling; event-scale; runoff and sediment yield; scenario simulation; SHETRAN

Funding

  1. Ministry of Business, Innovation and Employment
  2. University of Liverpool

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Changes in agricultural land use have significant impacts on downstream runoff and sediment generation. The spatial arrangement of riparian buffers and cropped fields does not influence event-scale flow and sediment yield. The use of post-harvest cover crops can significantly reduce modelled sediment yields.
Agricultural land use can increase runoff and erosion leading to detrimental downstream impacts. This paper examines the impact of agricultural land cover change on runoff and sediment generation at event scales using a model-based approach. SHETRAN, a physically based, spatially distributed model, was applied in two southwest England catchments to represent: (a) changes in the land cover (cropland extent and spatial arrangement), (b) changes in crop type and (c) use of riparian buffer strips. A total of 84 simulated events within a 4-year period were used to quantify impacts on flow and sediment generation. We found past changes in land cover resulted in significant differences in sediment yield (p < 0.05). Linear regression showed an increase in flow and sediment yield proportional to increases in arable crop area (p < 0.001). The spatial arrangement of cropped fields and riparian buffer strips produced no significant differences in event flow or sediment yield (p > 0.05). However, buffer strip scenarios compared with the base run showed sediment load reductions for specific events, up to 20% and 15% for woodland and grass riparian buffers, respectively. When comparing crop types with and without the use of post-harvest cover crops, we observed non-significant differences for event flow and sediment yield. However, large reductions in modelled sediment yields occurred for some events (e.g., up to 60% for winter cereals, 50% for maize and 74% for spring cereals). For these scenarios, examination of rainfall event magnitude emphasized the importance of ground cover in mitigating soil erosion for maize and spring cereals, but not for winter cereals. Our findings indicate that significant changes in sediment delivery at the event scale over a multi-year period are associated with variations in cropland extent and crop types, depending on rainfall magnitude, but not on the spatial arrangement of cropped fields or the use of riparian buffer strips.

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