Special Column:Celebration of the 70th Anniversary of IGSNRR, CAS

The Evaluation of Groundwater for the Water Source of Wuhai Thermoelectric Plant in Inner Mongolia

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  • 1. Shijiazhuang University of Economics, Shijiazhuang 050031, China;
    2. The First Institute of Hydrological and Engineering Survey, Inner Mongolia, Huhhot 010050, China

Received date: 2007-01-07

  Revised date: 2007-07-19

  Online published: 2008-02-01

Abstract

Based on the analsis of the hydrogeological conditions of the survey region, the groundwater recharge and discharge quantity is calculated with water balance method. The result of calculation is negative balance. After groundwater mining, the water source being mainly from the increased recharge of the Yellow River. The pumping test and the numerical simulation show that the increased recharge of the Yellow River is 3.45×104m3/d. According to water level forecast, after the water source being developed for 20 years or for 2 years running under adverse hydrological and meteorological conditions, the lowering of both water level is less than one-tenth of the aquifer thickness. This indicates that a mining rate of 3×104m3/d is assured which can satisfy the water supply demand of the thermoelectric plant.

Cite this article

SHAO Ai-jun, CHEN Yu-xia, YANG Jian-xun, LI Wen-mei . The Evaluation of Groundwater for the Water Source of Wuhai Thermoelectric Plant in Inner Mongolia[J]. JOURNAL OF NATURAL RESOURCES, 2008 , 23(1) : 127 -135 . DOI: 10.11849/zrzyxb.2008.01.015

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