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- W278852078 abstract "Rills are major sources of sediment in eroding systems. This study investigated the roughness of erodingrills as affected by the slope gradient and runoff rate. In flume experiments, loess soil material wassubjected to simulated rainstorms. Roughness of the major rills was determined using digital elevationmaps. Results showed that rill bed roughness significantly increased with slope steepness but was notaffected by the runoff rate. Generally, three patterns of bed roughness could be distinguished: (i) a low-frequencycomponent indicating the convex/concave shape of the rill length profile. (ii) a high-frequencycomponent of undirected roughness with an amplitude proportional to slope steepness. (iii) a cycliccomponent that seemed to reflect a series of regularly spaced micro-headcuts. The frequency of the micro-headcutstended to decrease with slope steepness, the amplitude increased with slope steepness. The resultsindicate that rill bed roughness is a dynamic parameter that is affected by slope steepness." @default.
- W278852078 created "2016-06-24" @default.
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- W278852078 date "2013-11-14" @default.
- W278852078 modified "2023-09-27" @default.
- W278852078 title "Cyclic and Non-Cyclic Patterns of Bed Roughness in Eroding Rills" @default.
- W278852078 doi "https://doi.org/10.13031/2013.4845" @default.
- W278852078 hasPublicationYear "2013" @default.
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