作者：闫成云;

机构：甘肃省地质调查院 甘肃兰州730000

中文关键词：昌马水库;;地下水补给量;;变化;;分析;;疏勒河流域

英文关键词：Changma reservoir;groundwater recharge resources;variation;analysis;Shulehe River basin

中文摘要：通过对昌马水库运行前后不同时期疏勒河流域各盆地河水—地下水相互转化的论述,详细对地下水补给量及其各主要补给项的变化原因进行了对比分析,流域地下水补给资源总体呈减少趋势,地下水的补给条件与更新能力被削弱。昌马水库运行后,中游玉门踏实盆地地下水补给量大幅减少,比上世纪60年代、90年代末分别减少了3.11×108m3、2.95×108m3,下游安西敦煌、花海盆地地下水补给量小幅增加。中游盆地泉水溢出量大幅衰减,与60年代比削减了53.2%。

英文摘要：Through discussion of conversion between the river resources and groundwater resources of the main basins in the different period in the Shelehe River basin before and after the Changma reservoir running and comparative analysis the reason of variation of the groundwater recharge resources and the main recharge term,it is expounded that the total trend of the groundwater recharge resources is reduced,the recharge condition and renew capacity of the groundwater is weakened.After Changma reservoir running,comparing to 60s and 90s of the last century,the groundwater recharge amount of Tashi Basin in the middle reach reduced so great that the amounts reached at 3.11×108m3 and 2.95×108m3 respectively,the groundwater recharge amount of Anxidunhuang and Huahai basins is increased a little in the lower reaches.Comparing with the 60s of the last century,the spring overflow in front of Changma proluvial fan reduced about 53.2 percent.

[中文刊名]：甘肃地质 [出版日期]：2007-05-15 [CN]：62-1191/P [ISSN]：1004-4116

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