煤炭工程 ›› 2017, Vol. 49 ›› Issue (1): 63-66.doi: 10.11799/ce201701019

• 生产技术 • 上一篇    下一篇

煤系地层顶板岩溶地下水赋存特征研究

史先志,钱自卫,李通文,等   

  1. 永贵能源开发有限责任公司
  • 收稿日期:2016-03-17 修回日期:2016-04-04 出版日期:2017-01-09 发布日期:2017-04-13
  • 通讯作者: 史先志 E-mail:zslsxz@aliyun.com

Study on occurrence characteristics of karst groundwater in roof of coal strata in Xintian coal mine

  • Received:2016-03-17 Revised:2016-04-04 Online:2017-01-09 Published:2017-04-13

摘要: 为了查明新田煤矿煤系地层顶板灰岩含水层岩溶发育规律及地下水赋存特征,矿井采用可控源音频大地电磁法及实施水文地质补勘探查了岩溶发育规律|通过放水试验及连通试验查明了井田内断层导水性|取水样分析了地下水水化学特征。研究结果表明,新田煤矿煤系地层顶板岩溶发育深度可达到埋深412.82m,岩溶在平面上受地形、构造控制明显|井田边界F1断层为一不导水断层,是矿井水文地质边界,井田内断层具有导水性,是灰岩含水层向矿井采场充水的通道|大气降水对含水层具有补给作用,从而间接向采场补给。

关键词: 煤系地层, 岩溶, 发育规律, 地下水, 赋存特征, 补给规律

Abstract: Xin tian mine is located in guizhou karst development area, the karst aquifer affect mine safety production. Mine by means of controlled source audio-frequency magnetotelluric method exploration, water test, connectivity test and water the comprehensive geophysical and geochemical exploration methods such as chemical analysis found out mine embedded depth of karst development depth can reach 412.82 m, karst in the plane are controlled by topography, structure is obvious; Field boundary F1 fault for a guide water fault, is mine hydrogeological boundary, fault in mining field with hydraulic conductivity, is limestone aquifer to the mine stope filling water channel, atmospheric precipitation has a supply of aquifer, and indirectly to the stope supplies. The mine through the research on the rules of karst development, for mine offer a scientific basis for comprehensive control of karst underground water disasters.

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