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• W2564607384 abstract "The long-term and current volumes of sediment exported from stream banks were calculated as potential sources of sediment in a large pond located at the catchment outlet of a small agricultural lowland basin strongly affected by anthropogenic pressure in France. Bank erosion was measured over a short period using a network of erosion pins along a small stream (1400 m long) to quantify the material exported during a single winter (2012–2013). The material exported by this same stream over the last 69 years was quantified using an original approach involving the comparison of a compilation of three-dimensional historical stream redesign plans that date back to 1944 with the state of the banks in 2013 (differential global positioning system and LiDAR data). The results suggest that a global trend of material loss along the stream banks monitored by erosion pins, with an average erosion rate of 17.7 mm year−1 and an average volume of exported material of 75 t km−1. Over 69 years, this same stream exported an average of 36 t km−1 year−1, and the average loss of material from the banks throughout the whole catchment was estimated to be 14 t km−1 year−1. The contribution of bank material to the filling of the pond over the last 10 years is between 46% and 52% based on an extrapolation of erosion pin dynamics or between 27% and 30% based on the comparison of LiDAR data to the average historical profile extrapolated for the catchment. These results suggest that bank erosion represents a major source of sediment in degraded waters in traditionally understudied agricultural lowland catchments, where anthropogenic pressures are high." @default.
• W2564607384 created "2017-01-06" @default.
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• W2564607384 date "2017-02-10" @default.
• W2564607384 modified "2023-09-23" @default.
• W2564607384 title "Quantification of bank erosion in a drained agricultural lowland catchment" @default.
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• W2564607384 doi "https://doi.org/10.1002/hyp.11117" @default.
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