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大孔隙对土壤水分入渗特性影响的物理模拟试验

吴继强 张建丰 高瑞

农业工程学报2009,Vol.25Issue(10):13-18,6.
农业工程学报2009,Vol.25Issue(10):13-18,6.DOI:10.3969/j.issn.1002-6819.2009.10.003

大孔隙对土壤水分入渗特性影响的物理模拟试验

Physical simulation experiments of effects of macropores on soil water infiltration characteristics

吴继强 1张建丰 1高瑞1

作者信息

  • 1. 西安理工大学教育部西北水资源与环境生态重点实验室,西安,710048
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摘要

Abstract

The different size sands and macropores' mold were used to simulate the same macropores' depth and different effective surface macropores, and a novel soil column was designed to observe the 3D infiltration of macropore flow under the condition of ponding water. The results showed that there was high correlation between the time when the wetting front turned to flush and stable and the effective surface macropore. The cumulative infiltration was in line with the Kostiakov model while its parameters were associated with the effective surface macropores. Under certain conditions, macropores connectivity played the dominant role for the preferential infiltration in soil. The presence of macropores could lead to typical change of the center profile's wet area. In the end, the study gave a quantitative concept for the center profile's wet area increment and its mathematical model with the effective surface macropores. The accuracy of the model verified by experiments can meet the requirments.

关键词

入渗/土壤/水分/大孔隙/有效面孔隙度

Key words

infiltration/ soils/ water/ macropores/ effective surface macropores

分类

农业科技

引用本文复制引用

吴继强,张建丰,高瑞..大孔隙对土壤水分入渗特性影响的物理模拟试验[J].农业工程学报,2009,25(10):13-18,6.

基金项目

国家自然科学基金资助项目(50779055) (50779055)

农业工程学报

OA北大核心CSCDCSTPCD

1002-6819

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