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不同节理裂隙发育特征对废弃矿山岩质边坡稳定性的影响研究

王水华 于义军 梅红专 张磊 何文武 苟劲松

华南地质2025,Vol.41Issue(3):613-622,10.
华南地质2025,Vol.41Issue(3):613-622,10.DOI:10.3969/j.issn.2097-0013.2025.03.012

不同节理裂隙发育特征对废弃矿山岩质边坡稳定性的影响研究

Influence of Different Joint Fracture Characteristics on the Stability of Rock Slopes in Abandoned Mines

王水华 1于义军 2梅红专 2张磊 1何文武 1苟劲松1

作者信息

  • 1. 湖北省地质局冶金地质勘探大队,湖北 十堰 442000
  • 2. 湖北省地质局第八地质大队,湖北 襄阳 441000
  • 折叠

摘要

Abstract

The fissured high-steep rock slopes in abandoned mines pose a significant threat to the safety of nearby residents due to their instability and failure.To reveal the influence mechanism of different joint fissure characteristics on the stability of high-steep rock slopes,this study employs particle flow numerical simulation to analyze the effects of joint dip angle,spacing,and persistence on slope deformation damage.The simulation results indicate that stress concentration at the tips of joints that obliquely cut the slope surface easily induces vertical penetration of fissures along the joint axial direction,significantly reducing slope stability.Reducing joint spacing intensifies the interaction between adjacent joints,accelerates the penetration of rock bridges,and leads to large-scale instability of the slope.Meanwhile,an increase in joint persistence markedly decreases slope stability.As persistence increases from low to high,the damage modes of the slope mainly manifest as local deformation,preliminary formation of sliding surfaces,and overall sliding instability of the slope.The research findings analyze the influence of different joint fissure characteristics on slope stability from a mesoscopic perspective,providing a scientific basis for analyzing the damage evolution process of slopes in practical engineering and formulating mitigation plans.

关键词

岩质边坡/节理裂隙/颗粒流模拟

Key words

rock slopes/joint fracture/particle flow code simulation

分类

天文与地球科学

引用本文复制引用

王水华,于义军,梅红专,张磊,何文武,苟劲松..不同节理裂隙发育特征对废弃矿山岩质边坡稳定性的影响研究[J].华南地质,2025,41(3):613-622,10.

基金项目

湖北省地质局项目(编号:KJ2024-36) (编号:KJ2024-36)

华南地质

1007-3701

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