煤炭工程 ›› 2018, Vol. 50 ›› Issue (2): 100-104.doi: 10.11799/ce201802027

• 研究探讨 • 上一篇    下一篇

顶板风化基岩含水层富水特征与涌(突)水危险性预测

曾一凡1,李哲2,宫厚健2,郑金红1   

  1. 1. 中国矿业大学(北京)
    2. 中国矿业大学(北京)国家煤矿水害防治工程技术研究中心
  • 收稿日期:2017-12-18 修回日期:2018-01-10 出版日期:2018-02-20 发布日期:2018-04-23
  • 通讯作者: 李哲 E-mail:2521933950@qq.com

Characteristics of water abundance in the aquifer of weathered bedrock of 2-2 coal roof in Ningtiaota Coal Mine and prediction on water inrush risk

  • Received:2017-12-18 Revised:2018-01-10 Online:2018-02-20 Published:2018-04-23
  • Contact: li zhe E-mail:2521933950@qq.com

摘要: 为了解决柠条塔煤矿2-2煤层顶部普遍发育的风化基岩含水层突水危险性评价难题,在分析其风化基岩发育特征的基础上,深入挖掘地质及水文地质资料,提出了能够考虑风化程度的富水性评价指标体系,包括风化影响指数、含水层厚度、渗透系数、脆塑岩厚度比、单位涌水量和岩芯采取率,并以此为依托对风化基岩含水层进行了富水性评价。以更加精确地预测顶板导水裂隙带发育高度为目标,将实测数据用于对经验公式的校正中,得出了符合研究区实际情况的导水裂隙带发育高度计算公式。根据导水裂隙带高度计算结果对顶板冒裂安全性进行分区,结合富水性评价结果,对煤层顶板风化基岩裂隙含水层突水危险性进行了预测评价。

关键词: 风化基岩, 顶板含水层, 富水特征, 顶板突水, 导水裂隙带

Abstract: In order to solve the risk assessment of water inrush in the aquifer of weathered bedrock of coal seam roof in Ningtiaota Coal Mine. Based on the analysis of the development characteristics of the weathered bedrock, according to the geological and hydrogeological data, including the proposed water enrichment evaluation index system of the degree of weathering, including weathering index, aquifer thickness, permeability coefficient, brittle plastic rock thickness ratio, unit water inflow and core take rate, and on this basis of weathering the bedrock aquifer of water abundance evaluation. In order to predict the height of water-conducting zone of the roof more accurately, corrected the empirical formula according to the measured data, and obtained the formula for calculating the height of the water flowing fractured zone which accords with the actual situation of the study area. According to the calculated height of water-conducting zone, the safety of roof cracking is partitioned. Combined with the result of water abundance evaluation, the risk of water inrush from bedrock aquifer of coal seam roof is evaluated.

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