平顶山十三矿突水特征与原因分析  

Characteristics and Cause Analysis of Water Inrush in Pingdingshan No.13 Mine

作　　者：于辉光[1] 郭德勇[1] 吴建亭 

机构地区：[1]中国矿业大学(北京校区),北京100083 [2]平顶山煤业集团公司,河南平顶山467000

出　　处：《矿业安全与环保》2005年第1期1-3,共3页Mining Safety & Environmental Protection

基　　金：国家自然科学基金项目(40002010)

摘　　要：针对平顶山十三矿发生的2次较大突水事件,对突水机理及影响突水的相关地质因素、地质构造、水文地质、涌水水温和充水水源、导水通道进行了综合分析,指出突水原因是地质条件与工程因素共同作用的结果,为矿井治理方案的制定及深部开采水害防治措施的选择提供了科学依据。To counter two larger water inrush accidents occurred in Pingdingshan No.13 Mine, comprehensive analysis are made in this paper on the water inrush mechanism and the relevant geologic factors, geological structure, hydro-geology, the temperature of discharged water and water source affecting water inrush. The paper pointed out that water inrush resulted from the common action of the geological conditions and engineering factors, which thus provides the scientific basis for working up mine water control plan and choosing water control measures during deep mining.

关 键 词：矿井突水 充水水源 导水通道 突水机理 

分 类 号：TD745[矿业工程—矿井通风与安全]