新疆干旱内陆河灌区灌溉入渗分析  

Analysis of Infiltration in Irrigation Area of Arid Inland River in Xinjiang

作　　者：王俊[1] 姜卉芳[1] 马存林 何英[1] 

机构地区：[1]新疆农业大学水利与土木工程学院,新疆乌鲁木齐830052 [2]伊犁州喀什河流域管理处,新疆伊犁835000

出　　处：《水利与建筑工程学报》2007年第1期22-24,47,共4页Journal of Water Resources and Architectural Engineering

基　　金：国家"863"计划(2002AA2Z4201)

摘　　要：在新疆干旱内陆河灌区地面灌溉条件下,通过负压计、中子仪、地下水埋深监测研究,得出零通量面的形成变化规律、生育期田间水分变化及入渗;生育期间,土壤水和地下水相互转换关系活跃。Under the condition of surface irrigation in the irrigation area of arid inland river in Xinjiang, through the negative pressure gauge, neutron instrument and the monitoring research for embedded depth of groundwater, we can obtain the forming and changing regulation of ZFP and the moisture change and infiltration in field at childbearing period. The results show that the mutual change relation of soil water and subsoil water is active.

关 键 词：干旱内陆河灌区 生育期 田间水分变化 零通最面 入渗 

分 类 号：S274[农业科学—农业水土工程]