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.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.