重庆市高观塘滑坡的稳定性研究
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摘要
众所周知,滑坡是一种十分普遍的物理地质作用,它广泛涉及水电、铁路、公路、采矿等部门的工程建设,边坡失稳作为普遍的工程问题历来受到国内外学者的重视。对滑坡稳定性及变形机理进行研究,为合理有效的滑坡防治措施提供准确的参数,在工程实践中显得尤为重要。
     本文结合实际滑坡灾害的防治研究项目,以重庆市滑坡灾害较为严重的巫山县为背景,以典型的高观塘滑坡为研究对象,以为实际工程提供合理设计参数为目的,对高观塘滑坡的形成机理、稳定性影响因素和稳定性评价等进行了较为全面的研究,对今后巫山县地区类似滑坡的预防及稳定性分析具有良好的示范作用。论文的主要工作及内容如下:
     通过现场调查,滑坡勘探资料及室内外试验,对高观塘滑坡形成机理和形成条件进行了系统分析,研究表明人类工程活动是该滑坡产生的直接诱发因素,大气降雨是滑坡进一步加速发展的最主要因素。同时,高观塘平台的地层岩性、地质构造、地貌特征及水文地质条件等都是滑坡的主要形成条件。
     研究了高观塘滑坡的发育发展过程和变形破坏特点,运用自然历史分析法、极限平衡传递系数法及有限元法等多种定性、定量方法对滑坡的变形破坏及稳定性进行了系统的分析研究,得出结论:高观塘滑坡次级滑坡在天然状态条件下处于基本稳定~稳定状态,暴雨状态下处于不稳定状态;主滑坡在天然状态条件下处于稳定状态,暴雨状态下处于欠稳定状态。这些结论与实际情况相符合。
     给出了简要的防治方案建议:在排水措施的基础上,对次级滑体进行减载处理,对主滑体采用两级支挡。
Landslide as one important branch of slope calamity is largely involved in the hydraulic electric engineering and railway, highway, mining etc. The instability of slope as the general project question has been always paid attention to by domestic and international scholar. The need of reseach about stability and deformation mechanism is exigent, seeking rational and effective parameters for the measure of landslide support is particularly important in the project practice.
     This thesis based on the factual engineering of GaoGuanTang landslide in WuShan County of ChongQing Municipality. Deformation mechanism ,affected factors and the stability of the landslide are studied in this paper. It provides some experimental and theoretical basis for further studying in this field. Main points are shown as follows: The areal of geology, hydrogeology, engineering geology and mans activity are investigated about the GaoGuanTang landslide. The disaster of landslide is evaluated.
     Through examination and site investigation, and combine pioneering data, the deformation mechanism and the conditions are systematically analyzed. The paper put forward that the direct factor of the landslide happened is several projects of human, the rainfall is the main factor that the landslide caused to develop rapidly. Further, lithology about stratum , geological structure, topographical feather and hydrogeology condition are main conditions about the formation of landslide.
     It is researched of the development process about the landslide. The stability of landslide is analyzed by transfer coefficient and finite element method. Moreover, calculates the rock structure character and the thrust acting on the landslip on the basis of which a tentative preventative program is put forward.Draw some conclusions as follows: the secondary landslide is elemental stability or stability in native state, is instability in rainstorm; the main landslide is stable in native state, is understable in rainstorm. These conclusions correspond with the practical situation.
     There are simple schemes about prevention and cure in the paper. On the basis of measure about water, continue to deal the secondary landslide with decrement of load; to deal the main landslide with two-stage axle stop.
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