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入渗水矿化度对点源滴灌土壤水盐运移特征的影响

李莎 何新林 王振华 蒲胜海 杨广 汪宗飞

灌溉排水学报2009,Vol.28Issue(5):79-81,3.
灌溉排水学报2009,Vol.28Issue(5):79-81,3.

入渗水矿化度对点源滴灌土壤水盐运移特征的影响

Effects of Water Salinty on Soil Salt and Water Movement under a Point Source Drip Irrigation

李莎 1何新林 2王振华 1蒲胜海 2杨广 1汪宗飞2

作者信息

  • 1. 石河子大学节水灌溉重点试验室,新疆,石河子,832000
  • 2. 石河子大学兵团绿洲生态农业重点实验室,新疆,石河子,832000
  • 折叠

摘要

Abstract

This paper studies initially on salt and water movement affected by mineralization degree of infil-tration water under a buried trickle source through laboratory test. The results show that, at the same depth of soil,the higher the salinity of water,the greater for soil moisture and soil salinity profiles. At the same infiltration time,the higher the salinity of water,the greater for the migration distance of moist in the horizontal direction; Under point sources drip irrigation, the distance of wetting front transport is related drip time with a nonlinear correlation.

关键词

微咸水/点源滴灌/水盐运移/入渗水矿化度

Key words

brackish water/ point source drip irrigation/ water and salt migration/ the salinity of infiltration water

分类

农业科技

引用本文复制引用

李莎,何新林,王振华,蒲胜海,杨广,汪宗飞..入渗水矿化度对点源滴灌土壤水盐运移特征的影响[J].灌溉排水学报,2009,28(5):79-81,3.

基金项目

国家自然科学基金项目(40861027) (40861027)

新疆自治区"十一五"科技攻关重大项目(200731137-1) (200731137-1)

国家"十一五"科技支撑计划项目(2007BAC17B02) (2007BAC17B02)

灌溉排水学报

OA北大核心CSCDCSTPCD

1672-3317

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