摘要
以陕西关中地区马兰黄土为对象，通过对试验测定结果的分析，得到非饱和黄土（Ｑ＿３）的含水量与基质吸力相关关系的数学模式。
In this paper,the malan loess on Guanzhong area in Shaanxi province has been studiedand a mathematic model of correlation between water content and matrix suction of unsaturatedloess has been obtained through the analyses to the measured results of experiment.Analyses showthat the mathematic model can excellently demonstrate the relation between water content and ma-trix suction of Malan loess in a large varying range of matrix suction.
出处
《水土保持通报》
CSCD
北大核心
1995年第4期39-42,共4页
Bulletin of Soil and Water Conservation
基金
水利部水利水电科学基金
关键词
非饱和黄土
含水量
基质吸力
unsaturated loess
water content
matrix suction
