自然资源学报

自然资源学报 ›› 2008, Vol. 23 ›› Issue (1): 127-135.doi: 10.11849/zrzyxb.2008.01.015

• 资源评价 • 上一篇    下一篇

内蒙古乌海热电厂水源地地下水资源量评价

邵爱军1, 陈玉霞2, 杨建勋2, 李文梅2   

  1. 1. 石家庄经济学院,石家庄 050031;
    2. 内蒙古自治区第一水文地质工程地质勘查院,呼和浩特 010050
  • 收稿日期:2007-01-07 修回日期:2007-07-19 出版日期:2008-02-01 发布日期:2008-02-01
  • 作者简介:邵爱军(1960- ),男,教授,博士,研究方向为水资源与水环境。E-mail:shaoaijun@sohu.com
  • 基金资助:

    国家自然科学基金(40672163);河北省自然科学基金(D2004000480)资助。

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

SHAO Ai-jun1, CHEN Yu-xia2, YANG Jian-xun2, LI Wen-mei2   

  1. 1. Shijiazhuang University of Economics, Shijiazhuang 050031, China;
    2. The First Institute of Hydrological and Engineering Survey, Inner Mongolia, Huhhot 010050, China
  • Received:2007-01-07 Revised:2007-07-19 Online:2008-02-01 Published:2008-02-01

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被引次数

14 | 1

摘要： 在分析勘察区水文地质条件的基础上,用水量均衡法计算了该区地下水的补给量和排泄量,结果为负均衡。水源地开采后水源主要来源于黄河激发补给量,抽水试验和数值模拟表明黄河激发补给量为3.45×104m3/d。根据水位预测,水源地开采20年后和不利水文、气象条件下连续开采2年,水位下降值均不及含水层厚度的1/10,说明水源地开采量3×104m3/d是有保证的,可以满足电厂供水要求。

关键词: 水源地, 地下水资源, 水均衡, 激发补给, 数值模拟

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.

Key words: water source, groundwater resource, water balance, increased recharge, numerical simulation

中图分类号: 

  • P641.8