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深埋土岩接触带下导水裂隙带发育规律

白汉营 李文平 陈学军 黄翔

工程地质学报2017,Vol.25Issue(5):1322-1327,6.
工程地质学报2017,Vol.25Issue(5):1322-1327,6.DOI:10.13544/j.cnki.jeg.2017.05.019

深埋土岩接触带下导水裂隙带发育规律

DEVELOPMENT RULES OF WATER FLOWING & FRACTURE ZONE AT DEEP BURIED SOIL-ROCK INTERFACE DURING MINING

白汉营 1李文平 2陈学军 3黄翔1

作者信息

  • 1. 桂林理工大学 桂林 541004
  • 2. 桂林理工大学,地质资源与地质工程博士后流动站 桂林 541004
  • 3. 中国矿业大学 徐州 221116
  • 折叠

摘要

Abstract

This paper aims to find the reason for preventing the crushing and water inrush accidents under deep buried soil-rock interface at coal mine in Eastern China.It analyses the geological environment of fractured rock mass with high water pressure under deep buried sand-sandstone interface.It uses the measured data including the height of water flowing fractured zone and simple hydrological observations data of drilling hole.It examines the development rules of the height of water flowing fractured zone during mining under deep buried soil-rock interface using principal component analysis.The results show that:ratio of the height of water flowing fractured zone and mining thickness and waterproof coal pillar fits Boxlucas1 exponential function model.The thickness of weathered zone inhibits the height of water flowing fractured zone to some extent.But for the sand-sandstone interface,as the presence of adown penetration zone,the inhibitory effect of weathered rock on the height of water flowing fractured zone increases.

关键词

深埋土岩界面/导水裂隙带/压架突水/下渗带

Key words

Deep buried soil-rock interface/Water flowing fractured zone/Support crushing and water inrush/Adown penetration zone

分类

矿业与冶金

引用本文复制引用

白汉营,李文平,陈学军,黄翔..深埋土岩接触带下导水裂隙带发育规律[J].工程地质学报,2017,25(5):1322-1327,6.

基金项目

国家自然科学基金项目(41172290),桂林理工大学博士(后)启动基金项目资助. (41172290)

工程地质学报

OA北大核心CSCDCSTPCD

1004-9665

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