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- W1528076781 abstract "After formation, a rill may remain in the field for weeks or months contributing to a large percentage of the sediment production downstream. Recent findings show that the rill flow transport capacity of soil clods can be much different from that in overland flow depending on the prevailing discharges. It is then hypothesized that within the sedimentation area of a rill network, rill erosion is able to generate a layer of sediments whose granulometric characteristic should be different than that produced by interill erosion (i.e., by overland flow). To what extent these granulometric differences also lead to local disparities in the hydrological behaviour of the soil (e.g., infiltration rate), is uncertain. The aim of this work is (i) to determine the incidence of the sediments generated by rill erosion on the hydrological properties of the sedimentation area, and (ii) to evaluate the granulometric characteristic of these sediments." @default.
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- W1528076781 date "2009-04-01" @default.
- W1528076781 modified "2023-09-26" @default.
- W1528076781 title "Effect of sediments generated by rill erosion on soil hydrology at small spatial scale" @default.
- W1528076781 hasPublicationYear "2009" @default.
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