软弱土层的位置和坡角对分层土质边坡的稳定性影响研究

针对不同层数和软弱土层处于不同位置的分层土质边坡工程,采用FLAC3D有限差分数值计算软件,以安全系数和边坡位移等值线图为边坡稳定性的评价指标,运用强度折减法模拟分析不同坡角对每种分层土质边坡稳定性的影响。在分析每种分层土质边坡不同坡角下稳定性的基础上,得出安全系数的变化规律,进而细化边坡达到临界稳定的坡角范围,并在此范围内分析边坡稳定性。     

影响三维土质边坡稳定性的多因素耦合分析

基于强度折减法,考虑坡高、坡角、边坡长度和坡转角四个因素,通过ABAQUS软件建立三维模型以模拟复杂土质边坡的稳定性问题。结果显示,影响边坡稳定性的因素是相互关联的,其中坡高和坡角与边坡安全系数呈负相关关系;边坡长度对三维边坡的稳定性影响分为两种:当坡高、坡角较小时,安全系数与边坡长度的关系表现出先减小后变得平缓的趋势;当坡角和坡高较大时,安全系数随边坡长度的增大呈现先减小后增大的趋势,但总体变化幅度很小;在坡长较大、坡高和坡角较小时,坡转角会对边坡稳定性产生明显的影响。     

基于ANSYS的土质边坡稳定性分析

土质边坡的稳定性对各种工程的施工有着重要的影响。文章利用有限元软件ANSYS,采用强度折减法分析了某边坡在自然状态下的稳定性,研究了锚索对边坡的加固效应。研究结果表明:强度折减法适用于边坡的稳定性分析;土质边坡在锚索加固后,塑性区加深且发展得到限制,边坡安全系数和稳定性得到显著提高。     

基于Hoek-Brown强度折减法的边坡稳定性图表法研究

边坡稳定性图表为初步评价边坡的稳定性提供一种简单但却行之有效的途径。采用Hoek-Brown有限元强度折减法,提出一套求解Hoek-Brown准则下岩质边坡安全系数的稳定性图表。首先根据Hoek-Brown准则下岩体的正应力与剪切应力的关系,推导关于瞬时内摩擦角φ_i和瞬时黏聚力c_i的一种显示表达公式,进而实现基于Hoek-Brown准则的有限元强度折减法在数值计算中的实施。算例分析表明,该方法获得的边坡安全系数和滑动面位置是合理可靠的,且避免对瞬时强度参数φ_i和c_i的迭代求解。在此基础上,绘制求解b=45°和D=0条件下边坡安全系数的稳定性图表;进而提出分别用扰动权重影响系数f_D、坡角影响权重系数f_β来量化岩体扰动和边坡坡角对稳定性的影响,并绘制求解f_D和f_β的计算曲线。从而建立求解Hoek-Brown准则下岩质边坡安全系数的稳定性图表法。最后通过对2个工程实例的计算表明,采用本文图表法求解岩质边坡安全系数是合理可行的。     

坡面沉桩边坡动态稳定性三维极限上限分析

 采用极限分析上限法,建立土质边坡坡面沉桩动态稳定性三维计算模型,研究沉桩力、桩土间横向力等对边坡动态稳定性的影响。通过算例计算,对整个沉桩过程中边坡抗滑稳定安全系数的变化规律及其内在机制进行深入研究,并分析桩径、沉桩位置、坡角对边坡抗滑稳定安全系数的影响规律。结果表明：沉桩力对边坡稳定性产生不利影响,导致沉桩前期边坡安全系数持续降低;桩体穿过破坏面后,边坡安全系数由于桩身的抗滑作用而显著提高。桩径越大,沉桩前期安全系数越低,其下降速度也越快,但桩体穿过破坏面后安全系数提升也越明显;沉桩位置越靠近坡顶,沉桩过程中安全系数下降速度越快,导致最危险点的安全系数越低;坡角越大,沉桩过程中整体安全系数越低。分析结果对于坡面沉桩的稳定性评估及设计施工具有一定参考价值。     

边坡稳定性及安全系数确定研究

指出在边坡稳定性分析中,一般采用安全系数来衡量边坡的稳定性,并根据安全系数采取相应的边坡治理措施,因此边坡的安全系数取值大小对于边坡安全、工程效益有着直接影响,采用有限元分析法,利用ANSYS有限元分析软件,确定了安全系数范围,从而确定安全系数的大小。     

强度折减有限元法研究开挖边坡的稳定性

用强度折减有限元方法对开挖边坡的稳定性进行了较为全面的研究。分析结果表明 :当折减系数达到某一数值时 ,边坡内一定幅值的广义剪应变自坡底向坡顶贯通 ,认为边坡破坏 ,定义此前的折减系数为安全系数 ;和强度指标相比 ,弹性模量、泊松比、剪胀角和侧压力系数对边坡的安全系数影响不大 ;开挖边坡和天然边坡具有相似的破坏形式 ,表明强度折减有限元方法适用于开挖边坡的稳定性分析。最后指出 ,强度折减有限元法具有广泛的适用性和良好的应用前景     

基于ABAQUS的边坡稳定性分析

文章利用ABAQUS有限元软件模拟边坡,通过强度折减法,分析边坡弹性模量、边坡坡角、土体重度、C值、少值、土坡高度、剪胀角等各自不同取值对边坡安全系数的影响,得到相应的位移云图、关系曲线等,将边坡安全系数作为评定边坡稳定性的一个重要评判指标,达到降低边坡风险和滑坡、崩塌等自然灾害及时预警的目的,最大限度降低生命财产损失...     

基于有限元法对边坡稳定敏感性参数的分析

采用有限元强度折减法,从计算范围、内摩擦角、粘聚力、土体重度、坡高与坡度等方面,研究了计算敏感性参数对山区边坡稳定性安全系数的影响,结果表明,土体的粘聚力、内摩擦角和重度对边坡稳定性的影响最为敏感,坡角与坡高的影响次之,计算范围的影响最小。     

顺层岩质边坡稳定性分析

运用极限平衡法确定顺层岩质边坡在不同边坡角时的临界滑面,计算了临界滑面的安全系数,依据安全系数对边坡在不同边坡角时的稳定性进行了研究,并针对安全系数小于临界值1.35时的边坡角,研究了其在结构面倾角不断变化时,边坡安全系数的变化规律。     

圆形凸坡的稳定性分析

通过三维数值分析表明圆形凸坡的破坏模式接近于轴对称破坏,采用一般的三维破坏模式会使计算结果偏于不安全,揭示了目前三维分析方法中滑裂面形状的假设并非总是合理。构建了轴对称条件下的容许速度场,得到了内摩擦角(=0时圆形凸坡临界坡高的上限解。同时提出了轴对称破坏模式下,计算圆形凸坡安全系数的极限平衡方法。比较了圆形凸坡和长直坡的稳定性差异,圆形凸坡的相对半径越小、土体越接近于纯黏性土时两者的差异越大,坡度较小时前者较稳定,坡度较大时则相反,进而纠正了以往认为平面应变模型计算圆形凸坡偏于不安全的错误认识。     

Probabilistic stability analysis of earth dam slope under transient seepage using multivariate adaptive regression splines

Earth dams are widespread throughout the world and their safety has gained increasing concern from geotechnical engineering societies. Although probabilistic stability analysis approach has been widely applied to the safety assessment of geotechnical structures, few studies have been performed to investigate the effects of water level fluctuations on earth dam slope stability considering uncertainties of soil parameters. This study proposes an efficient probabilistic stability analysis approach by integrating a soft computing algorithm of multivariate adaptive regression splines (MARS). The calibration of a MARS model generally requires a large number of training samples, which are obtained from repeated runs of deterministic seepage and slope stability analyses using the GeoStudio software. Based on the established MARS model, the earth dam slope failure probability can be conveniently evaluated. As an illustration, the proposed approach is applied to the probabilistic stability analysis of Ashigong earth dam under transient seepage. The effects of the uncertainties of soil parameters and water level fluctuation velocity on the earth dam slope failure probability are explored systematically. Results show that the MARS-based probabilistic stability analysis approach evaluates the earth slope failure probability with satisfactory accuracy and efficiency. The earth dam slope failure probability is significantly affected by the water level fluctuation velocity and the coefficient of variation of the effective friction angle.

     

考虑土条间作用剪力的土坡稳定分析方法

本文通过对土条间作用力的方向、位于条间界面的剪切力作用形式进行了假定：认为条间界面的作用力满足水土平衡的最小承载力,而由此引出一个简单方程式,用以确定土条间作用力的夹角。依据平衡条件,结合强度破坏准则,解决土坡稳定分析中的全部未知数。     

基于SPH的土质边坡稳定性及失稳后大变形数值模拟

本文采用光滑粒子流体动力学(SPH)法对土质边坡稳定性及其失稳后的大变形进行数值模拟研究。该方法既可以分析边坡的稳定性系数和潜在滑移面,又可以对土质边坡失稳后的大变形过程进行模拟,从而弥补了传统数值模拟分析方法的不足,为土质边坡稳定性及失稳后滑坡大变形分析提供了一种新的方法。首先,采用Fortran语言编写了模拟土质边坡稳定性及失稳后滑坡大变形分析的SPH程序;其次,采用一个经典算例,验证了本文程序和方法在进行边坡稳定性分析时的准确性;最后,为验证该法模拟黏性土质边坡滑坡大变形的准确性,笔者自行设计了一组黏性土体滑坡大变形物理实验并与SPH模拟结果进行了对比。研究成果表明,基于弹塑性本构模型及D-P屈服准则的SPH方法可以较准确的模拟稳定性系数及潜在滑移面,并且可以较准确地模拟失稳后的滑坡大变形发展过程,弥补了目前数值模拟方法的不足,是一种值得推广的新型稳定性及滑坡大变形分析方法。     

Instrumented model slopes to investigate the effects of slope inclination on rainfall-induced landslides

Rainfall infiltration is considered as one of the most significant factors triggering slope instability as a number of slope failure occurrences have been documented during or immediately after a rainfall. The rainfall-induced slope instability is governed by a complex interaction of topographical, hydrological and geological conditions of the slopes. Hence slope inclination is vital in determining slope stability under rainfall. Although studies have been carried out to investigate the mechanism of rainfall-induced slope failure, limited compelling experimental studies have been conducted on the factors influencing the initiation of slope failure. In this study, instrumented model slopes were subjected to artificial rainfalls to investigate the effects of the slope inclination on slope stability, and a validated numerical model was developed using the test results from the instrumented model slopes. The outcomes of the study prove that the slopes become more susceptible to sudden collapse during rainfall as the slope angle increases. Further, the results highlight that when the slope inclination is 1.2 times greater than the friction angle of the soil, the failure is initiated by the loss of soil suction, and when it is smaller than or equal to 1.2 times the friction angle of the soil, the failure is initiated by the positive pore water pressure developed at the toe of the slope.     

岩土工程稳定性分析RFPA强度折减法

将强度折减法的基本原理引入到岩石破裂过程分析RFPA方法中，建立RFPA—SRM岩土工程稳定性强度折减分析方法。该方法以有限元方法作为应力分析工具，不仅满足静力平衡、应变相容，且充分考虑材料的细观非均匀特性，并秉承RFPA方法的破坏过程分析优势，能够反映岩土结构随强度劣化而呈现出渐进破坏诱致失稳的演化过程。以岩土工程中的边坡为例，阐述RFPA-SRM方法在边坡稳定性分析中的应用。利用RFPA—SRM方法进行边坡稳定性分析时，不需对滑动面做任何预先假定，对复杂地质地貌的边坡稳定性分析是实用的；同时以基元的破坏次数统计作为边坡的失稳判据，不仅可直观地得到坡体的滑移破坏面，还可求得安全系数，为边坡的稳定性研究提供一种新的便捷、有效方法。特别是RFPA-SRM对边坡破裂过程的模拟对于理解边坡的破坏形成机制具有重要意义，更有利于从边坡失稳的源头入手指导边坡防护设计。最后对RFPA-SRM方法在一连拱分叉隧道安全设计中的应用进行探讨，得到该隧道结构的安全系数及潜在破坏模式，表明RFPA-SRM方法同样适合其他岩土结构稳定分析。     

考虑降雨影响的非饱和土基坑边坡突变失稳分析

降雨入渗往往是非饱和土基坑边坡失稳的主要诱发因素之一,同时边坡失稳又具有突发性。基于突变理论提出了考虑降雨入渗影响的非饱和土基坑边坡稳定性分析方法。根据分析边坡稳定性的塑性极限方法的上限理论建立了边坡失稳尖点突变模型,并得出边坡突发式滑坡的特征关系式,用突变理论对非饱和土边坡稳定进行了初步研究。研究表明,基坑边坡失稳是一种突发性的破坏,外界环境的变化(如降雨入渗导致土体抗剪强度的降低)是基坑边坡发生突发性破坏的决定性因素。     

土工格栅均布加筋土坡稳定性分析的上限解法

根据塑性极限分析理论，考虑格栅的加筋效应，对土工格栅均布加筋土坡的稳定性进行了上限解法；由此，确定了格栅加筋土坡临界高度的上限和稳定数。井与无加筋情况下边坡的计算结果进行了对比分析；通过变动参数，计算分析了格栅加筋土坡坡角、表面坡角、土的内摩擦角及格栅抗拉强度对加筋土坡临界稳定数的影响。     

An experimental investigation on slope stability under drawdown conditions using transparent soils

This paper presents an experimental investigation into slope failure during water-level drawdown using transparent soil. The internal characteristics of slope failure are not well-known due to the limitations of the techniques used in the experiments conducted to date. In this study, transparent soil is used to visualize the process of slope failure. We developed a water-level control system to implement simulation of the drawdown of the water level at various speeds and used a charge-coupled device camera to capture images during the entire slope failure process. Particle image velocimetry was used to measure the displacement of the sand particles and identify the sliding zones. The flow paths of the fluid inside the slope were illuminated using an organic dye. The results show that the slope failure process can be divided into two stages: surface and overall sliding. The overall sliding of the slope is caused by the gradual development of partial instability, and the failure mode is a cyclic failure. The slope angle is different above and below the water level during the process of sliding. In our experiments, the slope angle is about 20° above the water level, which is the same as the final stable slope angle, and about 35° below the water level, which is the same as the initial slope angle. This means that the drawdown influences the angle above the water level but has little influence on the angle below the water level. The results of this paper provide a better understanding of the physical behavior and failure mode of soil slopes caused by drawdowns near the coast.