曲面边坡破坏特性及机理的对比试验

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL Bulletin of Engineering Geology and the Environment Pub Date : 2023-08-19 DOI:10.1007/s10064-023-03379-x
Shuwei Sun, Jiabing Hu, An Deng, Xianfu Xu, Hui Ding
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引用次数: 0

摘要

许多滑坡发生在曲面斜坡上。曲面具有加速边坡破坏的潜力,对露天矿边坡和矿山排土场边坡的分析具有重要意义。对弯曲边坡进行合理的分析需要对其破坏和变形行为有一定的了解,而这一点目前还没有得到充分的阐明。本研究在重力载荷条件下,对凹截面面和凸截面面的边坡进行了一系列基础摩擦模型对比试验。开发了一种改进的散斑分析和位移测量系统,用于捕捉地基摩擦模型试验中边坡的变形和破坏过程;因此,考虑形状和曲率的影响,对边坡破坏过程的行为和机理进行了研究。结果表明,凹段和凸段边坡均经历了明显的逐步破坏过程。滑移面是由弯曲边坡变形局部化的发展引起的,凹断面边坡的滑移面近似为弧形,初始变形发生在坡顶;凸断面边坡的滑移面近似为线状,变形首先发生在坡面中部。边坡的变形破坏过程可分为均匀变形阶段、应变局部化阶段和破坏阶段三个阶段。提供了两个特征试验时间来说明弯曲边坡的稳定性,表明凹剖面边坡的稳定性高于凸剖面边坡,这与其他结果基本一致。采用有限元方法,利用用户编写的程序对具有曲面的边坡进行应变局部化分析,并采用体积应变和最大剪切应变分析了曲面边坡的变形机理。提出了一种新的指标来分析试验中作用于边坡的体积效应和剪切效应的相对程度,表明凹剖面边坡的剪切效应在边坡的顶部区域更为明显,而凸剖面边坡的剪切效应在边坡表面的中间区域更为明显。结合强度折减法和有限差分程序FLAC3D,采用数值模拟的方法分析了带曲面边坡的滑移面几何形状和位置。数值模拟得到的曲面边坡破坏特征与基本摩擦模型试验结果基本一致。此外,对于具有凹、平面和凸断面面的边坡,边坡的滑移面逐渐由圆形破坏转变为近似线性破坏。在工程实践中,陡坡或局部变形可能是运动的标志,是露天矿和排土场边坡破坏的前兆。研究结果可为进一步认识曲面边坡的破坏特征和破坏机制、早期识别边坡的滑坡危险性提供有力支持。
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Comparative tests on the failure characteristics and mechanisms of slopes with curved surfaces

A number of landslides have occurred in the slopes with curved surfaces. Curved surfaces have the potential to accelerate the failure of slopes and are essential for the analysis of slopes as open pit slopes and waste dump slopes in mines. Reasonable analysis of curved slopes requires knowledge about their failure and deformation behavior, which are not thoroughly clarified so far. In this study, a series of base friction model tests were conducted comparatively on slopes with concave and convex section surfaces under gravitational loading conditions. An updated speckle analysis and displacement measurement system was developed to capture the slope deformation and failure process in the base friction model tests; thus, the behaviors and mechanism of the failure process of the slopes were studied considering the effect of shape and curvature. The results showed that both the concave and convex section slopes experienced a significant step-by-step failure process. The slip surface was caused by the development of deformation localization in the curved slopes, and the slip surface of the concave section slopes was nearly arced with an initial deformation at the crown, while for the convex section slopes, the slip surface was nearly linear and the deformation occurred first at the middle of the slope surface. The failure behavior was significantly influenced by the shape and curvature of a slope surface, and the deformation and failure process of slopes was divided into three phases: the uniform deformation phase, the strain localization phase, and the failure phase. Two characteristic test time are provided to illustrate the stability of curved slopes, demonstrating that the stability of concave section slopes was higher than that of convex section slopes, which was basically consistent with the other results. A strain analysis was conducted to investigate the strain localization of the slopes with curved surfaces by user-written code following the finite element method, and the deformation mechanism of the curved slopes was analyzed by volumetric strain and maximum shear strain. A novel index was proposed to analyze the relative degree of volumetric effect and shear effect acting on slopes during the test, which indicates that the more pronounced shear effect of the concave section slopes appeared in the crown area of the slope, while the significant shear effect appeared at the middle of the slope surface for the convex section slopes. The slip surface geometry and location of the slopes with curved surfaces were illustrated by numerical modeling combining the strength reduction method with the finite difference program FLAC3D. The failure characteristics of slopes with curved surfaces obtained from numerical modeling were nearly consistent with the base friction model test results. Furthermore, it was found that for slopes with concave, planar, and convex section surfaces, the slip surface of the slopes gradually transformed from circular failure to nearly linear failure. In engineering practice, scarps or local deformation could be signs of movements and thought of precursors of open pit and waste dump slope failures. These findings could provide solid support to understand the failure characteristics and mechanism and early identify landslide hazards of slopes with curved surfaces.

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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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