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贵州山区软基型弃渣场失稳机理探究

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贵州山区具有复杂的地质环境,弃渣场滑坡灾害屡见不鲜,文中依托贵州某高速公路YK9+180-YK9+480填方路基右侧B冲沟临时弃渣场遭遇连续强降雨后滑坡,通过现场地质调查、工程地质分析和构建地质模型开展数值模拟,分析该弃渣场滑坡机理.结果表明,弃渣场上覆较厚粉质黏土层,未清理便进行弃渣,由于沟谷排水不畅、汇水严重,降雨后粉质黏土基层及坡脚隆丘受浸泡形成软基,无法承受来自上部弃渣不合理堆填形成的巨大下滑力,受剪破坏形成灾害性滑坡;下部滑面为受强风化灰岩面控制的直线形滑面,中上部滑面为受均质弃渣体控制的圆弧形滑面.
Study on Landslide Mechanism of Spoil Ground with Weak Foundation in Guizhou Mountain Area
The mountainous areas of Guizhou have complex geological environments,and landslides in waste disposal sites are not uncommon.Based on the landslide of a temporary waste disposal site on the right side of the filling roadbed of a highway in Guizhou Province after continuous heavy rainfall,through on-site geological investigation,engineering geological analysis,and the construction of a ge-ological model,numerical simulations were carried out to analyze the landslide mechanism of the waste disposal site.The results showed that the waste disposal site was covered with a thick layer of silty clay,and the waste was disposed of without cleaning.As a result of poor drainage and severe water collection in the valley,the silty clay base and slope foot hills were soaked after rainfall,forming a soft foundation that could not withstand the huge sliding force caused by the unreasonable filling of the upper waste,resulting in catastrophic landslides due to shear damage.The lower sliding surface was a linear sliding surface controlled by the strongly weathered limestone surface,while the middle and upper sliding surfaces were arc-shaped sliding surfaces controlled by homogeneous waste material.

spoil ground with weak foundationslide failurenumerical simulationinstability mecha-nism

李蔚霖

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贵州省交通规划勘察设计研究院股份有限公司 贵阳 550081

软基型弃渣场 滑坡破坏 数值模拟 失稳机理

2024

交通科技
武汉理工大学

交通科技

影响因子:0.495
ISSN:1671-7570
年,卷(期):2024.(5)