黄土的大孔隙特征和大孔隙流研究  

Characteristics of Macro-pore and Macro-pore Flow in Loess Soil

作　　者：张建丰[1] 林性粹[1] 王文焰[2] 

机构地区：[1]西北农林科技大学,陕西杨陵712100 [2]西安理工大学,陕西西安710048

出　　处：《水土保持学报》2003年第4期168-171,共4页Journal of Soil and Water Conservation

基　　金：国家自然科学基金资助项目(49871038)

摘　　要：介绍了大孔隙流的概念和研究进展,对大孔隙的类型和在水文学上的分类方法进行了分析,并对大孔隙在土壤水分运动中的作用以及理论模式进行了探讨,分析了黄土的大孔隙发育特征和类型。论述了黄土区大孔隙流研究的必要性。The concept of macro-pore flow and relevant research in the macro-pore flow was generally described, and the type and classification method of the macro-pore was analyzed. The function of the macro-pore in the soil water movement and the relevant theory were discussed. And the developing feature of the macro-pore and the type were analyzed in loess area. Moreover, the necessity of the research in the macro-pore flow in loess area is illustrated.

关 键 词：黄土 大孔隙 发育特征 类型 大孔隙流 水文学 土壤水分运动 

分 类 号：S152.7[农业科学—土壤学]