Geomorphic considerations for erosion prediction

Environmental Geology
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Abstract

Current soil-erosion prediction technology addresses processes of rainsplash, overland-flow sediment transport, and rill erosion in small watersheds. The effects of factors determining sediment yield from larger-scale drainage basins, in which sediment movement is controlled by the combined small-scale processes and a complex set of channel and other basin-scale sediment-delivery processes, such as soil creep, bioturbation, and accelerated erosion due to denudation of vegetation, have been poorly evaluated. General suggestions are provided for the development of erosion-prediction technology at the geomorphic or drainage-basin scale based on the separation of sediment-yield data for channel and geomorphic processes from those of field-scale soil loss. An emerging technology must consider: (1) the effects on sediment yield of climate, geology and soils, topography, biotic interactions with other soil processes, and land-use practices; (2) all processes of sediment delivery to a channel system; and (3) the general tendency in most drainage basins for progressively greater sediment storage in the downstream direction.

Suggested Citation

Osterkamp, W.R., Toy, T., 1997, Geomorphic considerations for erosion prediction: Environmental Geology, v. 29, no. 3-4, p. 152-157, https://doi.org/10.1007/s002540050113.

Publication type Article
Publication Subtype Journal Article
Title Geomorphic considerations for erosion prediction
Series title Environmental Geology
DOI 10.1007/s002540050113
Volume 29
Issue 3-4
Year Published 1997
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Environmental Geology
First page 152
Last page 157
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