The model is adapted to be used in semiarid regions . this article presents wudaogou test site to carry on modeling simulations . based on the results of " four waters " conversion at wudaogou test station , groundwater evaporation and infiltration have been evaluated furthermore 本文选取五道沟实验区进行模型验证，并在五道沟实验站“四水”转化关系研究成果的基础上，对潜水蒸发和入渗补给作了进一步的分析研究。
The annual water consumption of these oases and their seasonal variations , water consumptions for different land uses , water uses by social - economy and natural ecology , water balance and components of water consumption in farmland , recharge and consumption of groundwater as well as the classification of groundwater evaporation are quantitatively studied 取得了包括绿洲年耗水水平、绿洲耗水的年内分布、绿洲各类土地的耗水、社会经济与自然生态系统耗水比例、农田土壤耗水平衡与耗水组成、地下水补给与消耗的组成及潜水蒸发的分类等的初步定量结果。
Evaporation varies from evaporation capability , embedded depth of groundwater is more easy , the effect is more obvious ; evaporation capacity decreases if embedded depth of groundwater become deeply , and close to zero under the some depth ; evaporation capacity of different soil texture is different . at ordinary situation , if embedded depth of groundwater is easy , evaporation capacity of the wide and grit soil is powerful ; if embedded depth of groundwater is deep , evaporation capacity of the slender and viscosity soil is powerful 潜水蒸发随大气蒸发能力的变化而变化，且潜水埋深越浅，受其影响越明显：潜水蒸发随潜水埋深增加而减少，在某一埋深以下潜水蒸发接近于零：不同土质其潜水蒸发量不同，一般情况下，在潜水埋深较小时，土质较粗、偏砂性土壤潜水蒸发较大；当潜水埋深较大时，土质较细、偏粘性土壤的潜水蒸发较大。
In this dissertation we research the inversion pattern of three water through environment isotope information analysis , evaporation pattern analysis and inversion analysis of groundwater ; quantitatively analyse inversion amount through rule computational method and numeric value imitation , supplying scientific foundation for evaluation of water resources and rightful development and use 论文通过环境同位素信息分析、潜水蒸发试验分析、近河岸地带地下水动态分析研究三水转化规律特征；采用常规计算方法和数值模拟方法，定量分析地下水各转化资源量。为研究区水资源评价及合理开发利用提供了科学依据。
