摘要
针对平朔安太堡三号井工矿突水灾害,通过地质分析、河道渗漏观测、钻探、抽水试验等综合方法,依据井上、井下水中NO3-,NO3--N等离子特征分析了井下突水机理,研究了井下突水与地表平鲁区生活排污水、平鲁化肥厂排水及矿井排水之间的内在关系,初步查清了富水区及强富水带,为矿井防治水提供了依据。
According to the water inrush disaster occurred in No. 3 Deep Mine of Pingshuo Antaibao, with the geological analysis, water leakage observation of the river channel, drilling exploration, water pumping test and other comprehensive methods, the paper analyzed the underground mine water inrush mechanism base on the NO3^- , NO3^- - N plasmas in the surface water and underground water. The paper studied the inner relationship between the underground inrush water and the residential drainage water from Pinglu surface area, the drainage water from the Pinglu Fertilizer Plant and the mine drainage water. The rich water area and the ultra rich water zone were preliminarily clarified, which could be the references to the mine water control.
出处
《煤炭科学技术》
CAS
北大核心
2009年第4期103-105,128,共4页
Coal Science and Technology
基金
国家重点基础研究发展计划(973计划)资助项目(2007CB209402)
教育部"新世纪优秀人才支持计划"资助项目(NCET-06-201)
关键词
风化裂隙带
顶板型突水
水化学特征
河道渗漏测量
weathered fissure zone
water inrush from roof
water chemical features
measurement of river bed water leakage
作者简介
巩文胜（1964－），男，山西大同人，高级工程师，现任平朔煤炭工业公司安太堡三号井工矿总工程师，长期从事煤矿生产及安全管理工作。联系人：陈忠辉，Tel：13718167683，E—mail．cumtbczh@163．com
