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基于板壳和断裂力学理论的上覆采空区积水危险性判定技术

题正义 张峰 秦洪岩 朱志洁

煤田地质与勘探2019,Vol.47Issue(1):138-143,6.
煤田地质与勘探2019,Vol.47Issue(1):138-143,6.DOI:10.3969/j.issn.1001-1986.2019.01.021

基于板壳和断裂力学理论的上覆采空区积水危险性判定技术

Risk judgment technology of water accumulation in overlying goaf based on plate shell and fracture mechanics theory

题正义 1张峰 1秦洪岩 2朱志洁1

作者信息

  • 1. 辽宁工程技术大学矿业学院,辽宁 阜新 123000
  • 2. 华北科技学院安全工程学院,北京 101601
  • 折叠

摘要

Abstract

In order to avoid the threat of water penetration from the goaf of overlying seam No.6 during mining seam No.10 in Shengli coal mine of Linfen, Shanxi, plate-shells theory and fracture mechanics theory were used to establish the mechanics model of the development height of water-conducting fissure zone and the rupture depth of the floor. The water conducting fissure zone developmental height in districts I-VI of coal seam 10 is 46.77 m, 48.86 m, 56.05 m, 56.14 m, 56.33 m and 55.20 m, and the rupture zone depth of the floor in districts I-IV areas of coal seam 6 is 1.57 m, 1.14 m, 1.85 m and 1.26 m. By structuring criteria for water accumulation risk classification of overlying goaf and to determine the risk of accumulated water in the goaf of coal seam 6 during the mining process of coal seam10, the determination result shows that the water accumulation risk in districts I-IV areas of coal seam 6 is of the type of water inrush for seam 10, and would threaten the mining of coal seam10. The influence of the unminable area of seam 6 on the districts V-VI of seam 10 is of permeability of primary rock, and wouldn't threaten the coal extraction in the districts V-VI of coal seam 10.

关键词

采空区积水/板壳理论/断裂力学理论/导水裂隙带/破裂带

Key words

goaf water/plate-shell theory/fracture mechanics theory/water-flowing fractured zone/fractured zone

分类

矿业与冶金

引用本文复制引用

题正义,张峰,秦洪岩,朱志洁..基于板壳和断裂力学理论的上覆采空区积水危险性判定技术[J].煤田地质与勘探,2019,47(1):138-143,6.

基金项目

国家自然科学基金项目(51704148) (51704148)

煤田地质与勘探

OA北大核心CSCDCSTPCD

1001-1986

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