基于梯度塑性模型的多孔介质应变局部化分析的基本理论   总被引：5，自引：1，他引：4  

张洪武  秦建敏  刘国震 《岩土力学》2006,27(1):1-6

讨论了引入梯度塑性模型情况下的含液多孔介质双重内尺度律的特征以及相互作用问题。在引入梯度塑性本构模型的情况下,一方面材料应变局部化分析数值结果的正则性得到保证;而另一方面,含液多孔介质会出现双重内尺度律参数的共同作用问题。本文给出了此时内尺度律预测的一个基本方法,并对稳定性问题进行了分析,讨论了不同情况下实波速存在的条件,给出了对于给定的渗透系数情况下实波速存在的波数区间,并对相关现象进行了解释。  相似文献   

基坑土体侧向卸荷真三轴试验研究   总被引：15，自引：4，他引：11  

何世秀  朱志政  杨雪强 《岩土力学》2005,26(6):869-872

对武汉地区具有代表性的粉质粘土,用基坑开挖过程中坑周土体的应力路径在真三轴上进行模拟试验,得到平面应变条件下固结不排水卸荷试验结果,将其整理成应力-应变关系曲线、孔隙水压力-竖向应变关系曲线、中主应力系数-竖向应变关系曲线和卸荷试验应力路径图。试验结果表明,竖向( )压力不变,侧向( )卸荷时,其应力-应变关系随固结压力的增加,由应变硬化型向应变软化型转化;固结压力较低时,表现为剪胀,固结压力较高时,表现为先剪缩,后剪胀;当中主应力( )始终大于但接近于侧向压力( ),按所定义的中主应力系数bd值较稳定;有效应力路径随固结压力增大产生偏转。这些结论为进一步研究粘性土中主应力的作用奠定了基础。  相似文献   

土工合成材料与土工合成材料加筋砂土的相关特性   总被引：14，自引：4，他引：10  

吴景海 《岩土力学》2005,26(4):538-541

目前土工合成材料加筋的理论研究明显落后于工程实践。为了指导土工合成材料的优选和研究加筋机理,以5种国产土工合成材料为加筋材料,它们分别是针刺无纺土工织物、涤纶纤维经编土工格栅、玻璃纤维经编土工格栅、双向塑料拉伸土工格栅和土工网,系统进行三轴压缩试验以比较各种土工合成材料对砂土的加筋效果。试验结果表明：（1）各种土工合成材料加筋砂土的抗剪强度和应力应变特性不同;（2）无纺土工织物适合用于允许大变形的加筋土工程,涤纶纤维经编土工格栅和塑料拉伸土工格栅均适合用于对变形有较严格要求的加筋土工程,玻璃纤维经编土工格栅适合用于对变形有严格限制的加筋工程,设计时需要较大的安全系数,土工网适用低等级的加筋土工程;（3）砂土对各种土工合成材料侧向收缩的约束作用差异显著。  相似文献   

低围压下冻结粉质粘土的三轴强度及变形分析   总被引：1，自引：0，他引：1  

孙星亮  汪稔  胡明鉴  胡建华 《岩土力学》2005,26(10):1623-1627

高围压和低围压对冻土的变形性能及力学指标有不同的影响。对冻结粉质粘土进行了3种负温、4种围压下的三轴试验。试验结果表明：在温度相同时,不同围压、不同应变速率下的应力-应变曲线具有相同的形态,其三轴抗剪强度与围压及温度有明显的线性关系,与应变速率成指数关系;变形模量与围压没有明显的相关关系,但与温度成线性关系,与应变速率成指数关系。而且从冻土结构角度分析了冻土变形及其强度表现的内在原因。  相似文献   

水库蓄水对库底沉降影响的数值分析   总被引：1，自引：0，他引：1  

王俊杰  朱俊高  王克东  徐建荣 《岩土力学》2005,26(10):1591-1596

抽水蓄能电站常采用沥青混凝土进行库底防渗护面处理,过快的蓄水速率和过大的蓄水水头可能导致库底护面开裂。以某抽水蓄能电站的上水库为例,用考虑Biot固结理论的平面有限元法,在依据沉降观测点实测资料优化确定地基土模型参数的基础上,分析了水库蓄水速率和蓄水水头对库底沉降量、沉降率及库底沥青混凝土应变率的影响。结果表明,蓄水速率对地基的最终沉降值影响不明显,而在蓄高水位历时内,地基的沉降增量和最大沉降率均与蓄水速率和蓄水水头有很好的相关性,沥青混凝土的最大应变率仅与蓄水速率相关。  相似文献   

平面应变条件下土工格室加筋垫层的变形分析   总被引：4，自引：0，他引：4  

张福海  俞仲泉 《岩土力学》2005,26(Z1):241-243

将铺设在软土地基上的土工格室加筋垫层看作具有一定刚度的梁板。地基上梁板的变形计算一般以弹理论的文克尔假定为基础。针对文克尔假定中不考虑水平抗力影响的问题,提出了考虑水平抗力的双参数法,并以该法应用于土工格室加筋垫层工法的变形分析。  相似文献   

An elastoplastic constitutive model for rockfills incorporating energy dissipation of nonlinear friction and particle breakage     

Mengcheng Liu  Yufeng Gao  Hanlong Liu 《国际地质力学数值与分析法杂志》2014,38(9):935-960

A new elastoplastic model is developed for rockfills within the general critical state framework incorporating the state parameter. Two state functions are proposed to characterize the evolution of volume dilation and strain softening of rockfills, and a modified breakage index based on the concept of Hardin's relative breakage is defined to describe the progressive crushing of rockfills. The nonassociated plastic flow rule is derived from a state dependent dilatancy equation, and it incorporates energy dissipation due to intrinsic nonlinear friction and particle breakage upon shearing. Thus, their couple effect on the plastic deviatoric and volumetric deformation of rockfills is taken into account in the current model. The numerical analyses are carried out for a series of drained triaxial tests on the modeled rockfills at various consolidation pressures and stress paths. The volume dilation/contraction and strain softening/hardening of rockfills are accurately predicted by the proposed model, and the particle breakage and nonlinear critical state shear strength of rockfills are also well captured. The research findings indicate that the current model is applicable to represent the complex stress–strain–volume change behavior of rockfills in general. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

Behavior of sand–rubber particle mixtures: experimental observations and numerical simulations     

Changho Lee  Hosung Shin  Jong‐Sub Lee 《国际地质力学数值与分析法杂志》2014,38(16):1651-1663

A series of laboratory experiments and numerical simulations are conducted to explore the characteristics of mixtures composed of sand and rubber particles of the same median diameter. The mixtures are prepared with different volumetric sand fractions (sf = V_sand/V_total). The experiment focuses on assessing the strain level on the characteristics of the mixture with the volume fraction of each component. Numerical simulations using the discrete element method are performed to obtain insight into the microscale behavior and internal mechanism of the mixtures. The experimental results show that the behavior of the mixtures is dependent on the relative sand and rubber particles composition with variation in the strain levels. The numerical simulation reveals the effect of the soft rubber particle inclusion in the mixture on the micromechanical parameters. In low sand fraction mixtures, a high shear stress along the contact is mobilized, and the stress state is driven to a more anisotropic condition because of the relatively high particle friction angle of the rubber. The rubber particles play different roles with the strain level in the mixture, including increasing the coordination number and controlling plasticity of the mixture in a small strain, preventing buckling of the force chain in an intermediate strain, and leading to contractive behavior in a large strain. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

An improved return‐map stress update algorithm for finite deformation analysis of general isotropic elastoplastic geomaterials     

Junjie Huang  Qi Peng  Ming‐Xiang Chen 《国际地质力学数值与分析法杂志》2014,38(6):636-660

This paper develops a novel return mapping algorithm for the numerical integration of general isotropic finite strain elastoplastic constitutive models for geomaterials. The constitutive formulation is founded on multiplicative decomposition of the deformation gradient. The logarithmic strain measure as well as the exponential approximation of the plastic flow rule is utilized to restore the standard infinitesimal format return mapping algorithm. Central to the algorithm is the exploitation of a set of three mutually orthogonal unit base tensors for the representation of constitutive relations and the corresponding integration of the rate form of the constitutive equations. The base tensors constitute a local cylindrical coordinate system in the principal space, which allows to formulate the return mapping algorithm in the three‐dimensional space and reduce the dimension of the problem to be analyzed from six down to three. With the proposed approach, direct determination of the principal axes and the transformation procedure between the general space and the principal space, as required in traditional spectral decomposition, are avoided. Furthermore, the matrices that are involved in the inversion evaluation take simple forms, leading to extremely easy inverse computation. As a result, the consistent tangent operator can be streamlined into a form simpler and more compact than those by conventional integration methods. Following the formulation of the integration procedure, a numerical experiment is performed to assess the accuracy and efficiency of the proposed algorithm. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   

Capturing the complete stress–strain behaviour of jointed rock using a numerical approach          下载免费PDF全文

Kamran Esmaieli  John Hadjigeorgiou  Martin Grenon 《国际地质力学数值与分析法杂志》2015,39(10):1027-1044

This paper presents the results of a series of numerical experiments using the synthetic rock mass (SRM) approach to quantify the behaviour of jointed rock masses. Field data from a massive sulphide rock mass, at the Brunswick mine, were used to develop a discrete fracture network (DFN). The constructed DFN model was subsequently subjected to random sampling whereby 40 cubic samples, of height to width ratio of two, and of varying widths (0.05 to 10 m) were isolated. The discrete fracture samples were linked to 3D bonded particle models to generate representative SRM models for each sample size. This approach simulated the jointed rock mass as an assembly of fractures embedded into the rock matrix. The SRM samples were submitted to uniaxial loading, and the complete stress–strain behaviour of each specimen was recorded. This approach provided a way to determine the complex constitutive behaviour of large‐scale rock mass samples. This is often difficult or not possible to achieve in the laboratory. The numerical experiments suggested that higher post‐peak modulus values were obtained for smaller samples and lower values for larger sample sizes. Furthermore, the observed deviation of the recorded post‐peak modulus values decreased with sample size. The ratio of residual strength of rock mass samples per uniaxial compressive strength intact increases moderately with sample size. Consequently, for the investigated massive sulphide rock mass, the pre‐peak and post‐peak representative elemental volume size was found to be the same (7 × 7 × 14 m). Copyright © 2015 John Wiley & Sons, Ltd.  相似文献