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The effect of conservation tillage on runoff erosivity and soil erodibility during concentrated flow
Author(s) -
Knapen A.,
Poesen J.,
Govers G.,
De Baets S.
Publication year - 2007
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.6702
Subject(s) - topsoil , surface runoff , tillage , environmental science , soil science , erosion , flume , soil conservation , crop residue , soil water , soil structure , hydrology (agriculture) , agronomy , geology , flow (mathematics) , geotechnical engineering , mathematics , agriculture , ecology , paleontology , geometry , biology
Crop residues in conservation tillage systems are known to cause both a reduction in the erosive runoff power and an increase in the topsoil erosion resistance. In this study, the relative importance of both mechanisms in reducing soil loss by concentrated flow erosion is examined. Therefore, a method to calculate the effective flow shear stress responsible for soil detachment in the presence of a residue cover is applied. The determination of effective flow shear stress is based on the recalculation of the hydraulic radius for residue treatments. The method was tested in a laboratory flume by comparing soil detachment rates of identical pairs of soil samples that only differ in the presence or absence of crop residues. This shear stress partitioning approach and a soil detachment correction were then applied to a dataset of soil detachment measurements on undisturbed topsoil samples from a no‐till field plot on a loess‐derived soil, sampled during one growing season. Results indicate that only a small fraction (10% on average) of the difference in soil detachment rate between conventional and conservation tillage can be attributed to the dissipation of shear forces on the residues. The remaining decrease in soil detachment during concentrated runoff after a two‐year application of conservation tillage can be explained by the increased dry bulk density and root and crop residue content in the topsoil that reduces soil erodibility. After correcting for the presence of residues, the temporal variability in soil detachment rates ( D r ) during concentrated flow for a given flow shear stress (τ) for both treatments can be predicted fairly well (R 2 = 0·87) from dry soil bulk density (DBD, representing consolidation effects), soil moisture content (SMC, representing antecedent rainfall conditions), the dry mass of organic material (OM, representing root growth and residue decomposition) and saturated soil shear strength σ s, sat using an equation of the form:$$ D_{\rm r} = [{\rm a}\exp (-{\rm b} \times {\rm OM}) - {\rm c} \times {\rm SMC} - {\rm d} \times {\rm DBD}]\left[\tau - ({\rm e} \times \sigma_{\rm s,sat} + {\rm f})\right] $$This study is the first to show that the effect of conservation tillage on soil detachment rates is a result of soil property modifications affecting soil erodibility, rather than a result of the surface residue decreasing flow erosivity. Copyright © 2007 John Wiley & Sons, Ltd.