In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 20, No. 6 ( 2019-06), p. 2886-2906
Abstract:
Steady state soil depth is proportional to the infiltration, but inversely proportional to the erosion rate, when erosion is gradual A quasi‐universal prediction of soil depth as a function of slope angle is generated for gradual erosion and landsliding While mean slope depths for gradual erosion and landsliding are similar, for the same total erosion rate, greater depths can be achieved in the latter
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2018GC008125
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2027201-7
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