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定水头补给半无限带状含水层矿坑涌水量评价

康志强 王增银 黄奇波 黄静 邱进峰

水文地质工程地质2009,Vol.36Issue(6):1-5,5.
水文地质工程地质2009,Vol.36Issue(6):1-5,5.

定水头补给半无限带状含水层矿坑涌水量评价

Prediction of the inflow water into a pit in a semi-infinite zonal aquifer under the condition of constant water head

康志强 1王增银 2黄奇波 1黄静 2邱进峰3

作者信息

  • 1. 中国地质大学(武汉)环境学院,武汉,430074
  • 2. 中国地质科学院岩溶地质研究所,桂林,541004
  • 3. 中冶集团武汉勘察研究院有限公司,武汉,430074
  • 折叠

摘要

Abstract

Based on the analysis of hydrogeological conditions of a calcite mine area in Guangxi Autonomous Region, China, a hydrogeological model was generalized, and a formula for a complete penetrating well flow in a semi-infinite zonal aquifer with a constant recharge water head has been deduced. The formula is used to predict the inflow of water into the pit. The traditional method of interferential wells is used to validate the evaluation result. The results show that both the results are extremely closed under the condition of large numbers of projection times. However, using the formula is more convenient compare the stacking method of interferential wells in terms of calculation methods.

关键词

半无限带状含水层/完整井/矿坑涌水量

Key words

semi-infinite zonal aquifer/ complete penetrating well/ inflow of mine

分类

天文与地球科学

引用本文复制引用

康志强,王增银,黄奇波,黄静,邱进峰..定水头补给半无限带状含水层矿坑涌水量评价[J].水文地质工程地质,2009,36(6):1-5,5.

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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