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Soil erosion by surface water flow on a stony, semiarid hillslope
Author(s) -
Nearing M. A.,
Simanton J. R.,
Norton L. D.,
Bulygin S. J.,
Stone J.
Publication year - 1999
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/(sici)1096-9837(199908)24:8<677::aid-esp981>3.0.co;2-1
Subject(s) - stream power , erosion , splash , hydrology (agriculture) , geology , shear stress , sediment , flow (mathematics) , geotechnical engineering , entrainment (biomusicology) , surface runoff , flow velocity , environmental science , soil science , geomorphology , mechanics , ecology , biology , philosophy , physics , meteorology , rhythm , aesthetics
Soil erosion on hillslopes occurs by processes of soil splash from raindrop impacts and sediment entrainment by surface water flows. This study investigates the process of soil erosion by surface water flow on a stony soil in a semiarid environment. A field experimental method was developed whereby erosion by concentrated flow could be measured in predefined flow areas without disturbing the soil surface. The method allowed for measurements in this study of flow erosion at a much wider range of slopes (2·6 to 30·1 per cent) and unit discharge rates (0·0007 to 0·007 m2 s−1) than have been previously feasible. Flow velocities were correlated to discharge and hydraulic radius, but not to slope. The lack of correlation between velocity and slope might have been due to the greater rock cover on the steeper slopes which caused the surface to be hydraulically rougher and thus counteract the expected effect of slope on flow velocity. The detachment data illustrated limitations in applying a linear hydraulic shear stress model over the entire range of the data collected. Flow detachment rates were better correlated to a power function of either shear stress ( r 2 = 0·51) or stream power ( r 2 = 0·59). Published in 1999 by John Wiley & Sons, Ltd.