摘要
介绍了土壤中大孔隙流的研究,并用一种简单的方法对土壤内的大孔隙和中小孔隙的饱和导水率进行分析,同时讨论了农田耕作层大孔隙流和Darcy流饱和导水率的变异情况。
This paper discribes the study of preferential flow in soil. A simple method is introduced to the quantitative fractions of the saturated conductivity for soil macro , meso and micro pores. The variations of saturated conductivity of preferential and Darcy flow are also discussed.
出处
《水科学进展》
EI
CAS
CSCD
北大核心
1998年第2期107-111,共5页
Advances in Water Science
基金
国家自然科学基金
关键词
孔隙流
饱和导水率
土壤
农田耕作层
macro pores
meso and micro pores
preferential flow
Darcy flow.