Assessment of areal water and tillage erosion using magnetic susceptibility: the approach and its application in Moroccan watershed
2019
Bouhlassa, Saidati | Bouhsane, Naima
Soil erosion constitutes a serious threat for sustainable agriculture in many countries. Magnetic susceptibility of soil is a fast, cheap, and non-destructive technique that could be used to quantify soil erosion or soil redistribution on a long-term scale. This study attempts to analyze the variation of magnetic susceptibility in soil profiles having the same lithology and climatic conditions, but different land uses and slope gradients in a subcatchment in northern Morocco. Soil cores were collected on forested, cultivated, and pasture lands. Each core was associated to a field unit (also called a homogeneous unit) characterized by a set of four cited erosion factors. The samples were measured for mass–specific low-frequency magnetic susceptibility (χₗf) and frequency-dependent magnetic susceptibility (χfd). The linear correlation of χₗf and χfd indicates the homogeneity of magnetic population in soil. It supports the use of empirical models based on comparisons of χₗf to predict the value of magnetic parameter after tillage homogenization and removal of soil material from the surface, and to estimate soil erosion or redeposition. The study built a methodology improving these empirical models and enabling a quantitative approach of the phenomenon. Two models, namely “tillage homogenization” (as improved in this study) and the proposed “simple correlation” result in globally similar estimates of erosion, while another model, the “simple proportional” model, underestimates it. The results give an estimate of long-term erosion (deposition) in sampled units and allow drawing of an areal soil redistribution map in the watershed.
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