干旱内陆河灌区灌溉入渗系数的测定与计算  

Measurement and Calculation of Irrigation Infiltration Coefficient in Arid Inland River Irrigation Area

作　　者：胡顺军[1,2] 田长彦[1,2] 宋郁东[1,2] 

机构地区：[1]中国科学院绿洲生态与荒漠环境重点实验室,乌鲁木齐830011 [2]中国科学院新疆生态与地理研究所,乌鲁木齐830011

出　　处：《灌溉排水学报》2010年第2期124-125,共2页Journal of Irrigation and Drainage

基　　金：国家重点基础研究发展计划(2009CB421302);中国科学院知识创新工程重要方向项目(KZCX2-XB2-03);中国科学院"西部之光"人才计划"联合学者";国家自然科学基金(40771043;40471020);新疆维吾尔自治区科技攻关重大专项(200731137-3)

摘　　要：在深入分析灌溉水入渗和再分布过程的基础上,依据包气带水量平衡原理,提出了一种根据土壤剖面含水率和同步地下水埋深资料计算灌溉入渗系数的方法。应用事例表明,方法简单可行,易于推广应用。Irrigation infiltration is the main source of ground water recharge in arid inland river irrigation area.Irrigation infiltration coefficient is an important index affecting the intensity of irrigation in farm field,its value is related to the assessment accuracy and utilization.In this the process of infiltration and redistribution of irrigation water,based on the principle of water balance,a method of calculating the irrigation infiltration coefficient is present,by using the soil moisture content of soil profile and depth of groundwater table at the same time.The case study shows that the method is workable and has practice value.

关 键 词：干旱内陆河灌区 入渗系数 水量平衡 土壤剖面含水率 地下水埋深 

分 类 号：S274[农业科学—农业水土工程]