温金梅, 倪化勇, 王春山, 王骏, 吴涛. 2018: 砂泥岩互层斜坡演化及失稳特征研究以三峡库区(长寿-丰都段)岸坡为例. 工程地质学报, 26(s1): 76-84. DOI: 10.13544/j.cnki.jeg.2018121
    引用本文: 温金梅, 倪化勇, 王春山, 王骏, 吴涛. 2018: 砂泥岩互层斜坡演化及失稳特征研究以三峡库区(长寿-丰都段)岸坡为例. 工程地质学报, 26(s1): 76-84. DOI: 10.13544/j.cnki.jeg.2018121
    WEN Jinmei, NI Huayong, WANG Chunshan, WANG Jun, WU Tao. 2018: STUDY ON THE EVOLUTION AND FAILURE CHARACTERISTICS OF THE INTERBEDED SLOPE OF SAND AND MUD STONESTAKING THE THREE GORGE RESERVOIR AREA(CHANGSHOU-FENGDU) AS AN EXAMPLE. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 76-84. DOI: 10.13544/j.cnki.jeg.2018121
    Citation: WEN Jinmei, NI Huayong, WANG Chunshan, WANG Jun, WU Tao. 2018: STUDY ON THE EVOLUTION AND FAILURE CHARACTERISTICS OF THE INTERBEDED SLOPE OF SAND AND MUD STONESTAKING THE THREE GORGE RESERVOIR AREA(CHANGSHOU-FENGDU) AS AN EXAMPLE. JOURNAL OF ENGINEERING GEOLOGY, 26(s1): 76-84. DOI: 10.13544/j.cnki.jeg.2018121

    砂泥岩互层斜坡演化及失稳特征研究以三峡库区(长寿-丰都段)岸坡为例

    STUDY ON THE EVOLUTION AND FAILURE CHARACTERISTICS OF THE INTERBEDED SLOPE OF SAND AND MUD STONESTAKING THE THREE GORGE RESERVOIR AREA(CHANGSHOU-FENGDU) AS AN EXAMPLE

    • 摘要: 斜坡失稳是地球表层夷平作用的自然现象,也是工程活动经常面临的地质问题。三峡库区(长寿-丰都段)属于典型的砂泥岩互层区,在调查基础上重点研究了砂岩夹泥岩坡、泥岩夹砂岩坡的斜坡结构、演化过程和失稳特征,引入地形凹凸度因子利用SOM神经网络模型对研究区内38个斜(滑)坡失稳指数进行定量计算。研究结果表明,区内砂岩夹泥岩坡与泥岩夹砂岩坡失稳机理呈现出一定差异性。砂岩夹泥岩坡中,侧凹地貌有利于汇水,固有的空间形态导致地下水可作为斜坡失稳的动力条件。泥岩夹砂岩坡中,地表水难以下切坚硬砂岩体,侧向侵蚀形成单面山,斜坡表面残留土体在雨水浸润后容易发生形成滑坡失稳。建议加强上砂下泥类型斜坡的防治。

       

      Abstract: Deformation and failure of the interbeded slope of sand and mud stones is a serious geological problem during the engineering construction. In this paper, taking the Three Gorges Reservoir Area(Changshou-Fengdu section) as an example, the slope structure, evolution process and failure characteristics are studied based on field investigation. And then the failure coefficients of the 38slopes were calculated based on the factor of topographic concave-convex degree and the SOM model. The results show that 70% of the slopes along the Three Gorges Reservoir Area(Changshou-Fengdu section) are consisted of mudstone interbeded with sandstone. There is a certain difference in the failure mechanism between the slope which consisted of mudstone interbedded with sandstone and the slope consisted of sandstone interbeded with mudstone. According to the failure mechanism and stability assessment, the failure coefficients of the 7slopes in Three Gorges Reservoir area(Changshou-Fengdu section) are bigger than 0.4,indicating comprehensive prevention methods should be adopted, especially for the slopes consisted of sandstone above and mudstone below.

       

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