胜利露天煤矿滑坡机理分析及成因探讨  

Mechanism Analysis and Causes Discussion of Landslide in Shengli Open-cut

作　　者：张艳博[1,2] 康志强[1,2] 李毅军[3] 

机构地区：[1]河北理工大学资源与环境学院 [2]河北省矿业开发与安全技术重点实验室,河北唐山063009 [3]河北省冶金矿山管理办公室,河北石家庄050011

出　　处：《工矿自动化》2010年第6期11-14,共4页Journal Of Mine Automation

基　　金：河北省自然科学基金资助项目(E2008000410);河北省自然科学基金资助项目(E2009000782)

摘　　要：针对胜利露天煤矿的滑坡现状,分析了露天煤矿滑坡形成的内在因素,即地形地貌、地层岩性、地质构造、软弱层对滑坡的影响,阐述了露天煤矿产生滑坡的诱发因素,即降水、地震和人为作用对滑坡的影响,以及土冻结对露天煤矿边坡的破坏作用,得出了滑破的发生与发展严格受地形、地层岩性和地质构造控制,且主要受软弱带和降雨诱发的结论,为进一步分析和评价胜利露天煤矿滑坡现象提供了基础研究。In view of landslide status of Shengli open-cut,the paper analyzed internal factors of landslide formation of open-cut,namely topography and geomorphology,formation lithology,geological structure and soft layer,expounded inducing factors of landslide distribution of open-cut,namely rainfall,earthquake and artificial action,and destructive action to slope of open-cut made by soilfrost.It drew conclusion that distribution and development of landslide is controlled by topography,formation lithology and geological structure rigorously and is induced by soft layer and rainfall mainly,which provides basis research for further analyzing and evaluating landslide phenomenon of Shengli open-cut.

关 键 词：露天煤矿 滑坡 边坡 稳定性 

分 类 号：TD824.71[矿业工程—煤矿开采]