采矿与安全工程学报 ›› 2015, Vol. 32 ›› Issue (3): 511-517.

• 论文 • 上一篇    下一篇

煤矿井巷上方大型老滑坡复活机理与致灾过程

  

  1. 1.太原理工大学地球科学与工程系,山西太原 030024; 2.山西冶金岩土工程勘察总公司,山西太原 030002
  • 收稿日期:2013-08-21 出版日期:2015-05-15 发布日期:2015-06-12
  • 作者简介:龙建辉(1972—),男,湖南省沅江市人,博士,副教授,注册岩土工程师,从事地质工程方面的研究。
  • 基金资助:

    山西省自然科学基金项目(2013011036)

Revival mechanism and disaster-causing process of old-large landslide on coal mine tunnel

  • Received:2013-08-21 Online:2015-05-15 Published:2015-06-12

摘要: 我国不少矿井直接坐落在高陡斜坡或老滑坡的坡脚,工程活动使边坡失稳或使老滑坡复活诱发地质灾害现象时有发生。对大型老滑坡而言,其复活变形持续时间长、滑移方向因应力场条件变化而改变、且具有多级非连续破坏等特征,给滑坡的稳定评价与科学防治带来难题。本文以朱家店煤矿滑坡为例,通过现场勘查和监测研究,详细查明了滑坡区工程地质条件、滑坡复活的各种诱发因素、滑坡的变形破坏特征以及工程活动与滑坡复活的时空关系等;在此基础上,对滑坡在井洞修筑、坡体堆载前后及坡脚开挖不同应力环境下的稳定性和变形特征进行了FLAC3D 数值模拟分析,再现了滑坡质点位移、塑性状态和应变增量的变化规律,以及滑坡下部采煤巷道的受力和位移的变化特征,所得结论与现场监测结果一致。

关键词: 矿区滑坡, 采空, 成因机理, 数值分析, 稳定性

Abstract: Many coal mines in China are located in the toe of high and steep slopes or old landslide. Engineering activities lead to the geological disasters of slope failure or the old landslide resurrection occasionally. As far as large old landslides are concerned, normally it has a long cycle time for resurrected deformation, with slip direction varying from the conditions of stress field, and multistage destruction bring non-continuous, which also bring many problems in stability evaluation and scientific prevention of the slope. Zhujiadian mine landslide was taken as an example in this paper to figure out the engineering geological conditions in the landslide area, revival factors of landslide, deformation failure characteristics, and the temporal and spatial relationship between the engineering activities and landslide revivification through field survey and long-term monitoring. Furthermore, FLAC3D numerical simulation has been conducted for analyzing the slope stability and deformation under different stress conditions, such as caves construction, before and after the gangue filling and slope toe cutting. Under these circumstances, the change law of landslide of particle displacement, plasticity status and the shear strain increment and the characteristics of stress and displacement in the coal roadway located in the toe of landslide have been recreated. The result is consistent with monitoring results in the field.

Key words: landslide in coal mine, gob, formation mechanism, numerical analysis, stability