安家岭二号井田构造控水作用及对底板突水影响分析

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英文篇名：Analysis on Water Control Role of Mine Structure and Its Impact on Water Inrush from Floor in Anjialing No.2 Shaft 中文刊名：中州煤炭 英文刊名：Zhongzhou Coal 作者：李德彬 ; 茌伟伟 英文作者：Li Debin1 ; Chi Weiwei2 (1.The School of Resources and Earth Sciences ; China University of Mining and Technology ; Xuzhou 221116 ; China ; 2.China Institute of Water Resources and Hydropower Research ; Beijing 100038 ; China) 中文关键词：构造控水 ; 含水层富水性 ; 底板突水 英文关键词：water controlling of tectonism ; water abundance of aquifers ; floor water bursting 出版日期：2011-06-25 机构：中国矿业大学资源与地球科学学院;中国水利水电科学研究院; 年：2011 期：06 出版单位：中州煤炭

摘要

构造薄弱带形成突水通道,是突水的决定因素,同时也是影响和控制地下水流场的主要因素。因此,查明矿区构造的性质与发育特征,研究矿区主要构造的控水作用以及构造薄弱带的含水层富水性和地下水径流情况,是预防矿井水害的关键。以安家岭二号井工矿井田为例进行分析,以期为矿区防治水工程及水资源规划利用提供重要的决策依据。
Tectonic weak zone forms a channel of water inrush,it is the determinant factor causing water inrush,and it is also the main factor which influences and controls underground water flow.Therefore,it is the key to prevent mine water damage that identifying the nature and development characteristics of structures in mine area,studying the water control role of major structures in mine area,and identifying the water abundance of the aquifer and groundwater runoff flow conditions in tectonic weak zone.In the paper,mine field of Anjialing No.2 Shaft was analyzed,which is hoped to provide an important basis for decision making to the mine water control works and water resources planning and utilization.

引文

[1]许增荣.“构造深度”及其与山区基岩裂隙水的关系[J].铁道工程学报,2001(3):101-108.
    [2]邵爱军,刘唐生,邵太升,等.煤矿地下水与底板突水[M].北京:地震出版社,2001.
    [3]胡宝林,宋晓梅,车遥,等.刘桥矿区多期构造复合断层导水性分析[J].煤炭科学技术,2002,30(8):50-53.