首页|降雨影响条件下滑坡滑移面深度力学机理研究

降雨影响条件下滑坡滑移面深度力学机理研究

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滑坡规律一直是地质灾害滑坡领域研究的热点,针对滑坡滑移面分布不明晰的问题,以滑坡理论中的滑移面深度为研究对象,建立了斜坡上饱和土层理论滑移面深度计算模型.根据平衡力学法,在滑动面控制函数的基础上,采用叠加原理推导并验证了满足模型边界条件滑动层的深度解析解,并建立了数值分析模型,通过数值分析研究含水率和剪切强度的关系.在以上研究基础上,以六盘水市多个滑坡体监测工程为背景,提出滑坡体现场监测试验的可行性研究方案.通过现场试验,对滑坡体滑坡变化规律进行研究,详细分析了滑坡体在不同降雨量环境下滑坡变化规律,发现降雨量累计值达到临界值会造成滑坡体发生滑坡,同时发现连续降雨造成滑坡体发生滑坡的可能性变大,以及含水率与土体的抗剪切力的相关性作用.研究了滑动层深度与内摩擦角和黏聚力的关系,表明引起滑动的饱和土层在坡脚处较深,到坡面上部逐渐变浅.
Study on depth mechanical mechanism of the sliding surface of the landslide under the influence conditions of rainfall
The law of landslide has always been a hot spot in the field of geological disaster landslide,aiming at the problem of unclear distribution of the sliding surface of the landslide,the depth of the sliding surface in landslide theory was taken as the research object.A theoretical calculation model for the depth of sliding surface in saturated soil layers on slopes was established.According to the equi-librium mechanics method,on the basis of the sliding surface control function,the depth analytical solution of the sliding layer satisfying the model boundary condition was derived and verified,and a numerical analysis model was established to study the relationship between moisture content and shear strength through numerical analysis.Based on the above research,a feasibility study scheme for landslide on-site monitoring test was proposed based on the background of multiple landslide monitoring projects in Liupanshui City.The landslide variation law of landslide body was studied through field tests.The variation law of landslide in different rainfall environments was ana-lyzed in detail,and it was found that the cumulative value of rainfall reaching the critical value would cause landslides,and it was found that the possibility of landslides in landslides caused by continuous rainfall increased,and the correlation between moisture content and soil shear resistance.The relationship between sliding layer depth,friction angle and cohesion force was discussed,and it was shown that the saturated soil layers causing sliding were deeper at the foot of the slope and gradually became shallower to the upper part of the slope.

rainfall conditionon-site experimentslope stabilityautomated monitoringmoisture content

赵智辉、杨金虎、康跃明、肖勇

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中煤科工集团重庆研究院有限公司,重庆 400037

降雨工况 现场实验 边坡稳定性 自动化监测 含水率

国家自然科学基金面上项目重庆市科技局自然科学基金中煤科工集团重庆研究院有限公司自立项目

52274092cstc2020jcyjmsxmX07932023ZDYF15

2024

能源与环保
河南省煤炭科学研究院有限公司 河南省煤炭学会

能源与环保

CSTPCD
影响因子:0.221
ISSN:1003-0506
年,卷(期):2024.46(3)
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