摘要
采用压力板法测定了非饱和黄土的基质吸力。结果表明,非饱和黄土的水分特征曲线可用幂函数关系描述;吸着水含量与毛细管水含量随基质吸力的增大而减小;
The matrix suction of unsaturated loess was measured with the method of pressure board. The result indicated that the feature curves of moisture content in unsaturated loess could be discribed with power function relation.The water content of attraction and capillary decreased with the increase of the matrix suction, which consisted of attraction and capillary powers.
出处
《西北农业大学学报》
CSCD
北大核心
1997年第3期55-58,共4页
Journal of Northwest Sci-Tech University of Agriculture and Forestry(Natural Science Edition)
基金
水利部水利水电科学基金
关键词
非饱和黄土
水分特征曲线
基质吸力
吸着力
unsaturated loess, feature curve of moisture content,matrix suction, attraction power, capillary power