干旱内陆河灌区地面灌溉条件下土壤水盐运动规律研究  

Study on Water and Salt Transport in Soil under Surface Irrigation Condition in Arid Inland River Irrigatson Region

作　　者：冯广平[1] 姜卉芳[1] 董新光[1] 周金龙[1] 李根[1] 

机构地区：[1]新疆农业大学水利与土木工程学院

出　　处：《灌溉排水学报》2006年第3期82-84,共3页Journal of Irrigation and Drainage

基　　金：国家"863计划"(2002AA2Z4201)

摘　　要：通过对干旱内陆河灌区田间土壤水、盐及地下水动态监测试验分析,结果表明:超大水量冬灌方式是导致灌区土壤盐渍化恶性循环的主要原因。对农田土壤盐分的定点实时监测,能够定量表征农田生态环境状况优劣;地下水位埋深变化,可警示农田盐渍化的演变,对调整灌溉定额采取预防措施有指导意义。According to dynamic analysis of monitoring experiment for soil water,soil salt and ground water transport in soil in arid inland river irrigation region. It is concluded that winter irrigation with exceedance water is the main reason for making for vicious circle of soil salinization. Regular monitoring in same point for soil salt in field can quantitative show state of ecology environment changing;Groundwater fluctuation can warn development of agricultural field salinization, It can help leader adjust irrigation quota and adopt preventing measure.

关 键 词：水盐运移 冬灌 水盐监测 干旱内陆河灌区 

分 类 号：S152[农业科学—土壤学]