Physical degradation of soils as a consequence of erosion on slopes subjected to different agricultural uses.
DOI:
https://doi.org/10.24310/BAETICA.1998.v0i20.506Abstract
In this paper we analice the grazing influence on the soil texture. We have observed clay, silt and sand fractions loss at the surface horizon, specially at the top of the slope, as well as a deposition process at the slope base. This process seems to be more intensive at the slope in which both higher charge grazzing and roture land are developed; whereas, the slope with the natural vegetation does not record important erosion process.
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