新疆伊吾河流域水资源转化特征的分析研究  

Analysis and Study on Characteristics of Water Resources Transformation of Yiwoo River in Xinjiang

作　　者：郭琳[1] 郭健[2] 张兵[1] 

机构地区：[1]新疆水利水电勘测设计研究院地质勘察研究所,新疆乌鲁木齐830052 [2]新疆昌吉学院,新疆乌鲁木齐830052

出　　处：《地下水》2012年第5期120-121,共2页Ground water

基　　金：水利部2008年公益性行业研究专项(200801050)

摘　　要：在地质构造运动作用下,形成的背斜与向斜组成的伊吾河流域的三个构造盆地,在水流搬运而带来的松散沉积物堆积在盆地,为地下水赋存奠定了良好的空间。伊吾河从其发源地至归宿地,自南向北径流过这三个盆地,时而地下水时而地表水,其间转化关系相当频繁,相当密切。运用地下水均衡和水均衡法,分别计算各盆地的进区水量、区间消耗量和出区水量及其地下水补排量,为进行流域水资源合理配置奠定基础,对流域水资源的合理开发利用、生态保护具有现实意义。The paper describes three anticline and syncline formed tectonic basins of Yiwoo River Basin with geological tectonic movements in details.The water flow brought loose sediments accumulated in the basin laid a good space for storing groundwater.From the origin to the destination,Yiwoo River is flowing over the three tectonic basins from south to north,with frequently transformation between the surface stream and groundwater.The paper is based on groundwater balance and the water-budget method to calculate the recharge and the drain of water flow and groundwater in the area of each tectonic basin,and the water consumption between three basins.Therefore,the conduct of rational allocation of water resources is based on the results which are meaningful for the rational utilization and development of the water resources,the ecological protection in the Yiwoo River Basin.

关 键 词：水资源转化关系 盆地 伊吾河流域 

分 类 号：TV213[水利工程—水文学及水资源]