新集一矿111311工作面突水机理探讨  

Probing into Water Inrush Mechanism in 111311 Face of No.1 Xinji Mine

作　　者：王厚柱[1] 丁厚稳[1] 

机构地区：[1]国投新集能源股份有限公司新集一矿,安徽淮南232171

出　　处：《矿业安全与环保》2002年第1期24-25,27,共3页Mining Safety & Environmental Protection

摘　　要：从水量、水温等方面对新集一矿111311工作面异常突水和突水机理进行了分析。认为该工作面突水水源主要为17#煤层顶板砂岩水、F038断层和附近裂隙充水以及少量13#煤层顶板砂岩水。Analysis was made on the abnormal water inrush and water inrush mechanism in No. 111311 working face according to water quantity and temperature and a conclusion was drawn that the water inrush in this face mainly came from the water in roof sandstone of No. 17 coal seam,the water in F038 fault and fractures around it,and a small amount of water in roof sandstone of No. 13 coal seam.

关 键 词：突水水源 突水机理 水量 水温 砂岩水 断层 

分 类 号：TD745.2[矿业工程—矿井通风与安全]