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《Journal of Glaciology and Geocryology》 2008-02
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Analysis of the Change of Groundwater Resources due to Water Allocation in the Irrigation Areas of the Middle Heihe River

WEI Zhi1,2,3,JIN Hui-jun1,LAN Yong-chao4,HU Xing-ling5,WU Jing-kui4,YANG Si-zhong1,2,JI Yan-jun1,2(1.State Key Laboratory of Frozen Soil Engineering,CAREERI,CAS,Lanzhou Gansu 730000,China;2.Graduate University ofChinese Academy of Sciences,Beijing 100049,China;3.Baiying Reconnaissance and Design Institute of Water and Electricity,Baiying Gansu 730900,China;4.Laboratory of Watershed Hydrology and Application Ecology,CAREERI,CAS,LanzhouGansu 730000,China;5.Gansu Hydrology and Water Resource Bureau,Lanzhou Gansu 730000,China)  
Groundwater is the influential irrigation resources for the middle reaches of Heihe River,and will be governed by the surface water after water allocation to the western and eastern Juyan Lake.Based on groundwater observation data,and using ordinary Kriging interpolation,the changes of groundwater tables and volumes before the 1990s and from 2004 to the 2005 a were analyzed.The analyses show that groundwater tables in Ganzhou District of Zhangye Municipality,Linze and Gaotai Counties had dropped 1.3~2.7 m with a local differentiation.Consequently the groundwater reserves declined by about 8.23×108 m3.This may be attributed to the reduction of transformation of surface water to groundwater,which accounts for 45 % of the total decrease,and the resultant enhanced exploitation of groundwater for agriculture irrigation in the middle reaches of Heihe River after the river runoff being substantially diverted.As a result,the volume of groundwater is decreasing and the groundwater resources are degrading in the Middle Heihe River.Currently,readjustment of the industrial structure and saving the agriculture water are significant measures to hold all environments stably.
【Fund】: 中国科学院知识创新工程重要方向项目(KZC-SW-229)资助
【CateGory Index】: P641.8
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