Abstract
Four independent techniques were applied for quantitative evaluation of soil redistribution rates within an arable slope and their spatial-temporal variability over the agricultural period. Such a complex approach allows mutual control and cross-validation of results, increasing their reliability. Sinuous pattern of the soil redistribution rate variation along the slope is associated with the specifics of a runoff formation and rill development in the slope hollow bottoms. Different temporal resolution of the techniques used has allowed making a rough estimation of contribution of individual events into total soil losses.
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