强化黄土高原土壤渗透性及抗冲性的研究  

The Study on Strengthening Anti-scourability and Penetrability of Soil in Loess Plateau

作　　者：朱显谟[1] 田积莹[1] 

机构地区：[1]中国科学院水利部西北水土保持研究所,陕西杨陵712100

出　　处：《水土保持学报》1993年第3期1-10,共10页Journal of Soil and Water Conservation

基　　金：870302国家基金8460041号课题总结

摘　　要：针对黄土高原土壤侵蚀的特殊性,首先从土壤渗透性和抗冲性的机理入手,对黄土高原黄土堆积的全过程进行了一定的平行研究,认为黄土与黄土区土壤的渗透性强和抗冲性弱的特征,完全与黄土沉堆方式有关,黄土堆积以后更由于植被的生长而使前者获得巩固和提高;并使后者得到相应的改善,这样就从根本上明确了本项目研究的理论依据和主攻方向。Based on the specificity of soil erosion in Loess Plateau, from theview of mechanism of soil penetrability and anti-scourability, the parallel study is made for the whole process of loess deposit in Loess Plateau. The results show that in loess and loess areas, the causes of soil penetrability strong and ahti-seourability weak are closely relative to loess deposit patterns. After the loess is deposited, because of vegetations growth, soil penetrability is improved, and anti-scourability occurs corresponding changes. This article put forward the theory basis and research direction for soil and water conservation.

关 键 词：土壤渗透性 土壤抗冲性 黄土高原 

分 类 号：S152.72[农业科学—土壤学]