Underground reserve capacity and groundwater level respond to water transfer from south to north in Shijiazhuang, China

被引：0
|
作者：
Zhang Guanghui [1 ]
Fei Yuhong
Liu Keyan
Hao Mingliang
Shen Jianmei
机构：
[1] Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazshuang 050061, Peoples R China
[2] Bureau Water Res Survey Hebei, Shijiazhuang 050031, Peoples R China
来源：
JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES | 2007年 / 18卷
关键词：
water transfer from south to north; underground reserve; restore of groundwater level; potential capacity and variation trend;
D O I：
暂无
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
The capacity of the underground reserve to be used is 19.11X10(8) m(3) and its infiltrative intension is from 6.88x10(4) m(3)/(d center dot km(2)) to 9.63x10(4) m(3)/(d center dot km(2)). The center level depth of Shijiazhuang groundwater funnel area will rise from 52.3 m to 39.9-40.8 m and the funnel area will reduce from 401 km(2) to 320-326 km(2) after 10 years, and the level will rise to 22.8-31.4 m and the funnel wea will reduce to 195-261 km(2) after 30 years, which is under the reserve condition of the water transfer from south to North and under reducing pumping and controlling rain-flood into recharge groundwater.
引用
收藏
页码：56 / 58
页数：3
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