摘要
简要介绍了保亭县甘什岭滑坡的形态、地层岩性、水文地质环境条件及地质构造等情况,分析了该滑坡的形成原因,并对其进行稳定性评价和危险性分析,稳定计算方法选用剩余推力传递法对滑坡稳定性加以试算,其计算结果与滑坡实际情况基本吻合。通过以上分析,可得以下结论:当滑坡在天然状态下时,稳定系数K的范围在1.17~1.26之间,此时滑坡处于稳定状态;当滑坡在饱水状态下时,稳定系数K的范围在0.99~1.03之间,此时滑坡处于滑移状态。
The paper briefly introduces the shape features,geological lithology,environmental conditions and geological structure of GanShenLing landslide in BaoTing county.Analyzed the formation cause of the landslide,and make a stability evaluation and risk analysis of it,It is used residual thrust method in the stability calculation to calculate for the stability of landslide,the calculation results and the landslide roughly tallying with the actual situation.Through the above analysis can draw the following conculsions:Under the natural state,the landslide is in steady state while the stability factor range between 1.17 and 1.26;Under the heavy rain state,the landslide is in sliding state while the stability factor range between 0.99 and 1.03.
引文
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