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群矿开采条件下山西潞安矿区的地下水流场变化

代锋刚 张发旺 王滨 韩占涛 么红超 胡博文

地球学报2018,Vol.39Issue(1):94-102,9.
地球学报2018,Vol.39Issue(1):94-102,9.DOI:10.3975/cagsb.2017.122002

群矿开采条件下山西潞安矿区的地下水流场变化

Changes of the Groundwater Flow Field of Lu'an Mining Area, Shanxi Province, under the Condition of Group Mining

代锋刚 1张发旺 2王滨 2韩占涛 1么红超 3胡博文3

作者信息

  • 1. 河北地质大学, 河北省水资源可持续利用与开发重点实验室, 河北石家庄 050031
  • 2. 中国地质科学院岩溶地质研究所, 广西桂林 541004
  • 3. 中国地质科学院水文地质环境地质研究所, 河北石家庄 050061
  • 折叠

摘要

Abstract

Multiple coal mining leads to regional aquifer structure damage, which has seriously affected the regional groundwater circulation and evolution trend and seems to be the root cause of groundwater resource shortage in the coal mining area. With the Lu'an mining area in Changzhi basin as an example and through field investigation, similar material simulation and numerical simulation method, the authors analyzed the damage of aquifer structure and its influence on groundwater circulation. Sand tank simulation test results were compared with the results of numerical simulation, and the results show that the fissure development formed by coal mining is basically restricted to complete bedrock, which causes bending deformation of the water bottom clay rock and forms interlayer drainage area, but this has little damage to Quaternary unconfined aquifer structure; Effective thickness of thinner parts of water-resisting layer leads to the disappearance of unconfined aquifer due to mining fissures cutting waterproof layers; Artificial "headward erosion" caused by coal mining causes the abstraction phenomenon of groundwater between the original isolation groundwater systems, and mine water recharge appropriately increases.

关键词

计算机模拟/物理模拟/相似材料模型/群矿开采/含水层结构

Key words

computer simulation/physical simulation/similar material model/multiple coal mining/aquifer structure damage

分类

矿业与冶金

引用本文复制引用

代锋刚,张发旺,王滨,韩占涛,么红超,胡博文..群矿开采条件下山西潞安矿区的地下水流场变化[J].地球学报,2018,39(1):94-102,9.

基金项目

本文由国家自然科学基金重点项目(编号:41130637)、河北省高等学校科学技术研究项目(编号:ZD2014023 (编号:41130637)

QN2015061)、河北省科技计划项目(编号:15273630)和中国地质科学院水文地质环境地质研究所重点实验室开放基金(编号:KF201605)联合资助.This study was supported by the National Natural Science Foundation of China(No.41130637),Col-leges Scientific Research Project in Hebei Province(Nos.ZD2014023 and QN2015061),the Scientific Research Project of Hebei Province(No.15273630),and Key Laboratory of Geological Research Institute Open Fund(No.KF201605). (编号:15273630)

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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