共查询到18条相似文献，搜索用时 281 毫秒
1.
剑桥模型沿球应力轴(p 轴)等向塑性体变硬化; 在日本广泛采用的关口 — 太田模型沿初始固结线( K0 线)不等向塑性体变硬化。三轴试验数据表明: 自 K0 状态向伸长方向剪切时, 前者方法计算的体积应变偏小, 而后者方法计算的体积应变偏大。 作者提出一种介于上述两者之间 、考虑初始应力各向异性(如 K0 固结)的不等向塑性体变硬化弹塑性模型。 为了使模型在三维应力下较好地反映土的强度和变形特性, 模型的剪切屈服准则使用 SMP 准则。模型的土性参数与剑桥模型一样, 其预测值与粘土实测值的比较表明, 提出的模型是简单合理的, 可望在实际工程计算中得到使用。 相似文献
2.
常规剑桥模型和修正剑桥模型是以正常固结和弱超固结土的三轴试验现象为基础建立起来的,且试样的初始应力状态为各向等压的球应力状态,将模型应用于K0固结状态的原状土必然引起不可忽略的系统误差。基于原状土K0固结线与等倾线之间的关系,在常规剑桥模型的基础上推导并得到了基于K0线的原状土剑桥模型和修正剑桥模型。在主应力空间中,该模型以K0固结线而不是以等倾线为轴线,因而能反映原状土的结构性和各向异性。既有试验数据的验证表明,与常规剑桥模型和修正剑桥模型相比,该模型能更合理的描述原状土的屈服和强度特性。 相似文献
3.
基于Wheeler土体各向异性旋转硬化法则,结合边界面理论,构造一个能够反映土体初始各向异性及加载后应力诱发各向异性的边界面本构模型,并借助ABAQUS软件提供的UMAT子程序接口,采用隐式积分算法--图形返回算法实现。通过对正常固结状态下（OCR=1）高岭土试样三轴不排水剪切试验进行模拟,并将模拟结果与ABAQUS自带的修正剑桥模型模拟结果进行了比较分析,表明本模型的模拟结果能够反映土体在偏压加载过程中产生的各向异性现象。在此基础上,采用本模型对中等超固结（OCR=4）高岭土试样三轴不排水剪切试验进行模拟,并再次与ABAQUS自带的修正剑桥模型模拟结果进行比较,表明本模型能够较好地反映中等超固结土在小应变情况下的非线性特性。相比于经典弹塑性模型,如修正剑桥模型,本模型的模拟结果更符合中等超固结土的变形特性。 相似文献
4.
以能量方程为基础推导出各向异性和小应变条件下弹塑性的本构方程,并将屈服面与修正桥模型和试验测得的屈服面进行了对比,表明新的屈服面比修正剑桥模型更接近试验结果,采用从初始应力到状态边界面的距离为参数的系数来修正硬化准则以模拟土体小应谱条件下的应力－应变特征。将新的本构模型编入有限元程序,对小应变试验进行了计算分析,计算结果表明,新的模型比修正剑桥模型能更好地反映土体的主要力学特性。 相似文献
5.
从岩土类材料极限应力状态线所致的各向异性出发,提出了应力空间变换的思想。以修正剑桥模型屈服面的中心为映射中心,给出了重塑土的应力空间变换、应力增量变换的公式, 并考虑了应力洛德角的影响。在变换应力空间中对修正剑桥模型进行了重新表述与改进,给出了基于应力空间变换的改进模型的具体应力应变计算式。通过4种应力路径的基于应力空间变换的改进模型与修正剑桥模型预测结果的对比,揭示了改进后模型的优越性：可以较好的反映各向异性的影响;可以很好地反映三轴伸长等应力路径的应力应变特性;可以反映 等路径所致的软化现象。 相似文献
6.
天然土体的初始各向异性通常可对其后继循环特性产生显著影响。现有考虑循环载荷作用的土体弹塑性模型,往往采用类似修正剑桥模型的椭圆形屈服面,已有研究表明,该椭圆形屈服面因其拉伸弹性区域偏大,针对天然K0固结状态的土体,其计算精度较差。基于新近提出的广义各向同性硬化准则,在边界面方程中引入初始各向异性张量,并采用空间滑动面破坏准则（SMP）的变换应力法,建立了能考虑饱和黏土初始各向异性的循环边界面塑性模型。分别针对等压和偏压固结的饱和黏土静、动三轴试验进行模拟,结果表明,该模型能合理反映土体的初始各向异性及其后继循环动力特性。 相似文献
7.
剑桥模型只适用于正常固结软黏土,不能描述不等向固结土的应力-应变行为的各向异性特性。基于剑桥模型,在其椭圆屈服面中引入各向异性张量和一个形状参数,建立了一个各向异性屈服面,提出了一个适用于等向和不等向固结软黏土的本构模型。各向异性张量的初始值由初始固结应力状态确定,其演化过程由一个与塑性剪应变和塑性体应变都有关的硬化法则描述。形状参数的引入保证了各向异性屈服面的灵活性和适应性。通过对Boston Blue黏土、高岭土和Otaniemi黏土的三轴试验结果的模拟,验证了模型的模拟能力。 相似文献
8.
为了研究粘土的各向异性对孔压生成的影响,在修正剑桥模型的基础上,采用关口-太田应力比概念、结合邢义川-郑颖人方程,构造了一个各向异性旋转屈服面,建立了一个各向异性弹塑性本构模型;据此推导出一个各向异性孔压表达式,该式可以考虑Lode角以及主应力轴的平面旋转对孔压的影响;并采用新的孔压表达式着重分析了三轴应力状态下Lode角旋转以及主应力轴旋转所造成的孔压发展,并对条形荷载下的平面应变各向异性粘土地基中的孔压发展进行了计算。计算结果表明,地基中由于Lode角旋转造成的孔压不明显,但在荷载边角位置主应力轴旋转造成的孔压不容忽视,尤其是在埋深相对较浅的位置。 相似文献
9.
修正剑桥模型是最早建立和得到广泛承认的经典土体弹塑性模型之一,但不能模拟应力路径转折时土体的应力-应变特性以及应力引起的各向异性。将旋转运动硬化理论引入到剑桥模型中,给出了椭圆屈服面的旋转运动硬化机制,在不增加任何模型参数的情况下,把等向硬化的修正剑桥模型扩展为旋转运动硬化模型。扩展的新模型既保留了单调加载时的等向硬化的特性,又能反映应力路径转折时土体的本构特性与应力诱发的各向异性,初步验证了模型的有效性。 相似文献
10.
受沉积历史的影响,实际工程中土体的初始应力往往呈各向异性,此时传统圆孔扩张理论的假定条件不再成立,故其适用性也受到限制。借助于FLAC有限差分数值软件,建立了以压力为圆孔扩张边界的二维圆孔扩张模型,从圆孔的变形、孔周土屈服范围、圆孔扩张产生的超静孔水压力分布等方面进行分析,获得在初始应力各向异性的条件下压力控制圆孔扩张过程土体响应规律。计算分析结果表明,初始应力各向异性时,压力控制的圆孔扩张孔口径向位移、塑性区分布、超静孔隙水压力影响范围各个方向不相等;塑性区的分布具有明显的方向性,塑性区最大半径位于孔周土体初始大主应力方向上,并且其值比在相同的扩张压力作用下各向同性初始应力条件下的塑性区半径大,因此传统的初始等应力条件下位移控制的圆孔扩张理论用于分析各向异性初始应力的工程是偏于不安全的。 相似文献
11.
Natural soils such as clays exhibit a variety of features including anisotropy, destruction and overconsolidation. In this work, a constitutive model that is able to replicate those salient features of natural clays is presented. The model is based on the classical S-CLAY1 model, where the anisotropy of the soil is captured through the initial inclination and rotation of the yield surface. To account for overconsolidation, a parabolic Hvorslev envelope is adopted. The compression curve of the reconstituted soil is taken as the reference to describe the structural of the soil. Parameters of the proposed constitutive model all have clear physical meanings and can be conveniently determined from conventional triaixal tests. Numerical examples using the proposed model to simulate overconsolidated natural soils are presented and compared with existing experimental data, demonstrating the capability of the model. 相似文献
13.
The paper describes and evaluates an incremental plasticity constitutive model for unsaturated, anisotropic, nonexpansive soils (CMUA). It is based on the modified Cam-Clay (MCC) model for saturated soils and enhances it by introducing anisotropy (via rotation of the MCC yield surface) and an unsaturated compressibility framework describing a double dependence of compressibility on suction and on the degree of saturation of macroporosity. As the anisotropic and unsaturated features can be activated independently, the model is downwards compatible with the MCC model. The CMUA model can simulate effectively: the dependence of compressibility on the level of developed anisotropy, uniqueness of critical state independent of the initial anisotropy, an evolving compressibility during constant suction compression, and a maximum of collapse. The model uses Bishop's average skeleton stress as its first constitutive variable, favouring its numerical implementation in commercial numerical analysis codes (eg, finite element codes) and a unified treatment of saturated and unsaturated material states. 相似文献
14.
Circular opening is commonly encountered in wellbore drilling of petroleum engineering, boring for cast-in situ pile installation, and tunneling excavation. This paper presents a rigorous solution for the elastoplastic responses of the anisotropic soft soil mass around a circular opening excavated under undrained and drained conditions. Both the anisotropic elastoplastic behavior and the 3D strength of the soft clay are incorporated in the present solutions. The well-established anisotropic critical state elastoplastic model S-CLAY1, which can represent the initial fabric anisotropy and stress-induced anisotropy of soft soil, is further modified by the Spatially Mobilized Plane criterion to consider the 3D strength of geomaterials. Then, the investigated problems, excavation of a circular opening under both short-term (undrained) and long-term (drained) conditions, are formulated as a system of first-order differential equations and are solved as initial value problems. The distributions of stress components and anisotropy parameters around the opening, the stress trajectory of a soil particle at the opening wall, as well as the stress–displacement curve at the opening wall are presented to investigate the elastoplastic responses of the opening. Extensive parameters show that the overconsolidated ratio and coefficient of earth pressure at rest (K0) have remarkable effects on the elastoplastic responses around a circular opening. 相似文献
15.
Many clay rocks have distinct bedding planes. Experimental studies have shown that their mechanical properties evolve with the degree of saturation (DOS), often with higher stiffness and strength after drying. For transversely isotropic rocks, the effects of saturation can differ between the bed-normal (BN) and bed-parallel (BP) directions, which gives rise to saturation-dependent stiffness and strength anisotropy. Accurate prediction of the mechanical behavior of clay rocks under partially saturated conditions requires numerical models that can capture the evolving elastic and plastic anisotropy with DOS. In this study, we present an anisotropy framework for coupled solid deformation-fluid flow in unsaturated elastoplastic media. We incorporate saturation-dependent strength anisotropy into an anisotropic modified Cam-Clay (MCC) model and consider the evolving anisotropy in both the elastic and plastic responses. The model was calibrated using experimental data from triaxial tests to demonstrate its capability in capturing strength anisotropy at various levels of saturation. Through numerical simulations, we demonstrate the role of evolving stiffness and strength anisotropy in the mechanical behavior of clay rocks. Plane strain simulations of triaxial compression tests were also conducted to demonstrate the impacts of material anisotropy and DOS on the mechanical and fluid flow responses. 相似文献
16.
The piezocone penetration test (CPTU) is commonly used as a fast and economical tool to identify soil profile and to estimate relevant material properties in soils ranging from fine to coarse-grained. Moreover, in the case of fine-grained soils (clays and silts), the consolidation coefficient and the permeability can be estimated through the dissipation test. Undrained conditions are commonly assumed for the interpretation of CPTU in fine-grained soils, but in soils such as silts, penetration may occur in partially drained conditions. This aspect is often neglected in data interpretation thus leading to an inaccurate estimate of soil properties. This paper investigates numerically the effect of partial drainage during penetration on the measured tip resistance and the subsequent pore pressure dissipation response contributing to a more accurate interpretation of field data. A realistic simulation of the cone penetration is achieved with the two-phase Material Point Method, modelling the soil response with the modified Cam-Clay model. The approach takes into account large soil deformations induced by the advancing cone, soil–water, and soil–structure interactions, as well as nonlinear soil behavior. 相似文献
17.
This paper proposes a semi-analytical solution of undrained cylindrical cavity expansion in anisotropic soils with both isotropic and frictional destructuration. The rigorous derivation based on the general form of the SANICLAY model with destructuration is provided following a standardized solving procedure, and the features of anisotropy and structuration are then invoked in the cavity expansion solution by adopting the non-associated hierarchical model. Cavity expansion tests in both structured and unstructured clays with various overconsolidation ratio are conducted to investigate the evolutions of effective stresses, excess pore pressure, anisotropic parameters and structuration factors during cylindrical expansion. The results show that the effective stresses at the cavity wall are lower after expansion and the cavity excess pore pressure is oppositely higher in structured clays with slightly smaller plastic regions. The evolutions of anisotropy for structured clays appear to follow similar patterns to unstructured cases, whereas the degree of anisotropy is further developed with gradual loss of inter-particle bonds. Finally, the proposed solution is applied to predict the limit pressure of pressuremeter tests in Bothkennar clay, showing its ability for interpretation of in situ testing data in natural structured clays. 相似文献
18.
Different phenomena influence the strength and volumetric behavior of unsaturated soils. Among the most important are suction hardening, hydraulic hysteresis, and the influence of volumetric strain on the soil-water retention curves. Fully coupled hydro-mechanical models require including all three phenomena in their constitutive relationships. Among these phenomena, suction hardening is the most influencing as it determines the apparent preconsolidation stress, the position of the loading-collapse yield surface, and the shift of both the isotropic consolidation and the critical state lines. In this paper, a fully coupled hydro mechanical model is presented. It is based on the modified Cam-Clay model but includes a yield surface with anisotropic hardening that takes account of the shift of the critical state line with suction. For highly overconsolidated materials, the sub-loading surface concept has been included in order to increase the precision of the model for these materials. The shift of the retention curves produced by volumetric strains is simulated using a hydraulic model based on the grain and current pore size distribution of the soil. 相似文献
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