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花岗岩高陡边坡稳定性的运动学分析方法

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花岗岩是地球上分布最广的岩石类型之一,其贯穿性辉绿岩脉结构面与局部破碎带发育的特点,影响岩体的稳定性,将对建筑场地构成安全隐患.围绕某花岗岩高陡边坡,通过立体投影与矢量代数理论建立的运动学分析方法,应用DISP软件,对边坡整体与局部破坏模式进行分析,对局部边坡稳定性进行计算.仅考虑贯穿性结构面条件下,南部、西部与北部边坡发生整体平面滑动、楔形体以及倾倒破坏的可能性非常小.同时考虑其它结构面时,则南部边坡局部楔形体发生破坏的可能性较大.进一步结合结构面力学参数,计算得到的楔形体稳定性系数满足规范要求.破坏模式与稳定性分析结果也得到了现场实际情况与边坡变形监测数据的验证.
Kinematic Analysis Method for Stability of High and Steep Granite Slopes
Granite is one of the most widely distributed rock types on Earth.Its characteristic of penetrating diabase veins and locally developed fracture zones affect the stability of the rock mass and pose a safety hazard to construction sites.A kinematic analysis method based on three-dimensional projection and the vector algebra theory was established to analyze the overall and local failure modes of a granite steep slope.The DISP software was applied to analysis the stability of the local slope.The probability of overall planar sliding,wedge shaped deformation,and toppling failure of the southern,western,and northern slopes is very low when only considering the condition of penetrating structural planes.When considering other structural planes sim-ultaneously,there is a higher possibility of the local wedge failure in the southern slope.Further combining the mechanical parameters of the structural plane,the calculated wedge stability coefficient meets the requirements of the specifications.The results of the failure mode and the stability analysis have also been verified by the actual on-site condition and slope deformation monitoring data.The explo-ration in this article will provide a reference for the failure mode and the stability analysis method of granite steep building slopes.

High and Steep SlopesGraniteKinematicsDestruction ModeSlope Stability

杨运林

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福建省地质工程勘察院,福州 350002

高陡边坡 花岗岩 运动学 破坏模式 边坡稳定性

2024

土工基础
湖北省土木建筑学会,中国科学院武汉岩土力学研究所,武汉市土木建筑学会

土工基础

影响因子:0.238
ISSN:1004-3152
年,卷(期):2024.38(6)