人民长江 ›› 2021, Vol. 52 ›› Issue (1): 96-101.doi: 10.16232/j.cnki.1001-4179.2021.01.016

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西江上游封开段花岗岩边坡变形破坏宏观判据研究

刘广宁, 黄长生, 齐信, 王芳婷   

  • 出版日期:2021-02-23 发布日期:2021-02-23

Research on deformation failure and macroscopic criteria of granite slope in Fengkai section of upper reaches of Xijiang River

LIU Guangning, HUANG Changsheng, QI Xin, WANG Fangting   

  • Online:2021-02-23 Published:2021-02-23

摘要: 为了查明西江上游封开段花岗岩类边坡地质灾害类型及发育分布特征,以1∶50 000面上调查为基础,取得了翔实的花岗岩类边坡地质灾害调查资料。据此对边坡破坏类型及失稳模式进行划分,对变形破坏机理进行分析,进而对破坏宏观判据进行研究,以作为区内花岗岩类边坡地质灾害早期识别依据。研究区共调查花岗岩地质灾害点87处,均为小型,以全风化和微风化灾害居多,多发育分布在50~220 m、25°~45°的边坡地带;风化程度对其变形破坏模式起到控制作用,总体可划分为“滑移(滑塌)、倾倒、崩落(坠落)”3种类型。风化程度、坡型特征、地形坡度、节理裂隙发育状况、宏观变形特征等5个因素可作为研究区花岗岩类边坡变形破坏模式及失稳前的宏观判据。研究区花岗岩地质灾害主要包括“软化崩解、累进性破坏、刚性破坏”3种变形破坏机理。其中累进性变形破坏机理覆盖了所有花岗岩地质灾害体,软化崩解机理主要体现在中-全风化花岗岩类边坡地质灾害中,而刚性变形破坏机理主要体现在微风化和球状风化花岗岩类边坡中。

关键词: 花岗岩类边坡; 地质灾害; 变形破坏机理; 宏观判据;

Abstract: In order to find out the types and developmental distribution characteristics of granite slopes in the upper reaches of Xijiang River,and research the deformation failure mechanism and macroscopic criteria,based on the 1:50 000 survey,we obtained the data of geohazards investigation for granite slope.The type and the instability mode were divided and the mechanism of deformation and failure was analyzed,so as to provide macro criteria for early identification of geohazards in granite slopes.A total of 87 geohazards were investigated in the study area,all of them were small.The vast majority of the geohazards were completely and slightly-weathered,most of them were distributed in the slope area of 50~220 m and 25~45 degrees.The weathering degree played a dominated role in the deformation and failure mode,and it can be divided into 3 types:slip(slump),dump,and collapse(fall).Five factors such as weathering degree,slope type,terrain slope,joint fracture development and macroscopic deformation can be used as macroscopic criteria in the study of deformation and failure mode of granite slope in the region.The geohazards in the study area included the three deformation and failure mechanisms of "softening disintegration,progressive destruction and rigid failure".The mechanism of progressive deformation was reflected in all granite geohazards,the mechanism of softening and disintegration was mainly reflected in the moderately and completely-weathered granite,the mechanism of rigid deformation and failure was mainly reflected in the slightly-weathered and spherical-weathered granite slopes.

Key words: granite slope; geohazards; deformation and failure mechanism; macroscopic criteria;