中国农业机械化科学研究院集团有限公司 主管

北京卓众出版有限公司 主办

晋西黄土残塬沟壑区坡面水分边缘效应

Slope Water Edge Effect in Loess Gully Area in Western Shanxi Province

  • 摘要: 对晋西黄土残塬沟壑区不同整地方式的水分边缘效应进行了分析研究,得出几点结论:①坡耕地距边5 m部位土壤水分含量高于距边2 m和地边缘部位,距边2 m和地边缘部位土壤含水量相差不大;②水平阶0~100 cm土层边缘、中部和根部3部位土壤水分含量相差不大;而100~200 cm土层3部位差异明显,根部含水量分别比中部和边缘部位高18%和68%;③阳坡鱼鳞坑0~100 cm土层距离边25 cm部位土壤含水量明显高于距边2 cm部位。研究成果可为该区的生态建设提供一定的理论依据。

     

    Abstract: Slope water edge effect in loess gully area in western Shanxi province was studied.The results as follows:first,the soil water content of slop farmland in 5 m edge space is higher than in 2 m edge space and the edge part,and the soil water content in 2 m edge space is similar with edge part.Second,the difference of soil water content between edge,middle and root part is not obvious in bench step land of 0~100 cm,but the difference is obvious in 100~200 cm,root water content than the middle part and the edge part respectively higher 18% and 68%.Third,25 cm edge space water content of scale pit in 0~100 cm layer is obviously higher than 2 cm edge space.This study could be served as guidance to ecological construction.

     

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