摘要
针对干旱地区平原绿洲水土资源利用的特点，建立了以土壤水为中心的农区－ 非农区水均衡模型，该模型在已知地表水引用的情况下，可以对农区，非农区以及农区与非农区之间的水分迁移转化进行分析。本文给出了叶尔羌河平原绿洲１９９３～１９９６ 年农区，非农区的潜水蒸发量。
According to the characteristics of the water and soil resources utilization of arid area plain oasis, a water equilibrium model of agriculture non agriculture area based on soil water movement is established. If the data of surface water diversion are known, the model can calculate water transfer in agriculture area and in non agriculture area as well as between they two. The groundwater evaporation in agriculture area and in non agriculture area as well as groundwater transfer from agriculture area to non agriculture area between 1993 and 1996 in Yerqiang River basin plain oasis are given.
出处
《灌溉排水》
CSCD
1999年第2期47-51,共5页
Irrigation and Drainage
基金
国家自然科学基金
关键词
干旱
平原绿洲
叶尔羌河
土壤水
农区
非农区
drought plain oasis Yerqiang River soil water agriculture area non agriculture area water equilibrium
