塔里木河南岸地下淡水资源分布特征及成因分析——以哈得4油田水源地为例  

ANALYZING ON FRESH GROUNDWATER DISTRIBUTION AND FORMING IN SOUTH BANK OF THE TARIM RIVER——HARDER 4 OIL-FIELD FRESH GROUNDWATER RESOURCE AS AN EXAMPLE

作　　者：叶义生[1] 张鸿义[1] 陈萍莉[1] 刘平[1] 侯谦儒[1] 李强[1] 喜英[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第一水文地质工程地质大队,新疆乌鲁木齐830091

出　　处：《新疆地质》2004年第3期244-247,共4页Xinjiang Geology

摘　　要：塔里木河南岸地下水资源,主要为受塔里木河控制的具有高矿化背景的地下水,在塔里木河洪水的淡化影响下,形成了一定范围的地下水淡化带.这种淡化水对油田供水具有战略意义,在一定程度上制约着油田建设的发展.通过对塔里木河南岸地下淡水资源的分布特征与成因分析,为塔河南岸地下淡水资源的合理开发与利用指明了方向.Groundwater in south bank of Tarim River was controlled by the river water quality and have high salinity. A desalting groundwater belt desalted by floodwater of Tarim River formed. This desalted groundwater zone plays an important role in the oil-field water supply and can promotes or restricts oil-field development. Studying on the distribution and its genesis of fresh groundwater in south bank of Tarim River will give the way for the exploration of the oil-field fresh groundwater resource.

关 键 词：塔里木河 地下淡水资源 淡水 淡化带 

分 类 号：P641.8[天文地球—地质矿产勘探]