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Shvoong Home>Science>Agronomy - Agriculture>Observation on Soil Moisture Dynamics of Rainfed Ridge-furrow Planting Field in Sandy Area ——Result Summary

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Observation on Soil Moisture Dynamics of Rainfed Ridge-furrow Planting Field in Sandy Area ——Result

Article Abstract by: TsingHua    

Original Author: Journal of Arid Land Resources & Environment
Four fields were designed to conduct ridge-furrow planting experiment in desert region, and soil gravimetric water content
rates of that four fieldsand a conventional flat-tillage field were observed. Field observations indicated: during rape growing period, soil water contents of ridge-furrow planting fields were higher than that of conventionalflat-tillage field, especially in plow layer (0~30cm); The fluctuation of soil moisture showed "two peaks-two valleys"type during rape growing period, and it could be divided into five phases :"soil moisture restoring stage-soil moisture slowly consuming stage-soil moisture restoring stage-soil moisture rapidly consuming stage-soil moisture restoring stage”. The soil moisture fast consuming stage was coincidedwith the quickly growing period of rape, in which soil gravimetric water contents in of ridge-furrow planting fields were higher than that of conventional flat-tillage;Compared with the conventional flat-tillage field, in the same depthlayer of the soil, the variation coefficient of ridge-furrow planting fields was smaller, the thickness of fast changing layer and active layer was smaller, the stable layer was closer to the surface of the soil, and the dry-wet fluctuation of the soil was smaller.This experimental research could provide references to adjusting tillage measure of rainfed field, optimizing land use structure, and preventing wind erosion in desert region.
Published: May 30, 2005
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