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Experimental and computational modeling of unsaturated soil behavior under true triaxial stress states.

机译:真实三轴应力状态下非饱和土特性的实验和计算模型。

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摘要

Previous elasto-plastic critical state-based constitutive models for describing the stress-strain behavior of an unsaturated soil are presented and numerically investigated. The basic framework of the existing models is an extension of the classical Modified Cam-Clay model, now defined in terms of four state variables: net mean stress, p = (sigma 1 + sigma2 + sigma3)/3 - u a; deviatoric stress, q = (sigma1 - sigma 3); matric suction, s = (ua - uw); and specific volume, v = 1 + e. Step-by-step procedures are outlined for integration of the constitutive relations in solving the incremental stress-strain behavior. Computational constitutive drivers are then implemented to allow for the numerical simulation of conventional triaxial compression (CTC) and triaxial compression (TC) tests. Simulations are obtained from both explicit and implicit, integration techniques. The computational algorithms support numerical analyses in a deviatoric (p : q : theta : s) stress plane, where theta (Lode-angle) is a third stress invariant, and by using a mixed control (stress- and strain-controlled) constitutive driver in conjunction with a Generalized Cam-Clay model within a constant-suction scheme. Additional integration levels are to be devised to accommodate the nonlinear nature of the function accounting for matric suction effects.; A servo-controlled true triaxial (cubical) testing device is modified to test 10.0 cm (4.0 in) per side, cubical recompacted specimens of unsaturated soil under varying matric suction conditions. Recompacted silty sand ( SM) specimens of Piedmont residual soil are tested following a multi-stage testing scheme by controlling the major, intermediate, and minor principal stresses. Matric suction states in the specimens are induced and maintained constant during true triaxial testing by using the axis-translation technique. Results from a series of drained, stress/suction-controlled CTC and TC tests are used for validation of the constitutive models proposed for an unsaturated soil under axisymmetric loading conditions, and the model enhancements proposed in the present work. In all cases, the incipient critical state condition was defined at approximately 12% of total shear strain. The agreement between observed and computed results in a recompacted silty sand (SM) is encouraging, suggesting that these models can be incorporated within FEM-based analyses of boundary value problems involving soils with significant changes in the negative pore-water pressure due to varying environmental conditions.; True triaxial testing data from a series of drained, stress/suction-controlled triaxial compression (TC), triaxial extension (TE ), and simple shear (SS) tests, conducted in the cubical testing setup, are used to evaluate the nature of major, minor, and intermediate principal strain response of 10.0 cm (4.0 in) per side, cubical recompacted silty sand (SM) specimens under varying matric suction conditions, and for shear stress paths not achievable in a conventional cylindrical apparatus. The influence of matric suction on the shape, size and position of the failure envelopes in the octahedral (sigma1 - ua : sigma2 - ua : sigma3 ua) and principal (sigma 1 - ua : 2 (sigma2 - ua) : 2 (sigma3 - ua)) stress planes is also analyzed from the true triaxial testing data.
机译:提出并描述了基于弹塑性临界状态的本构模型,用于描述非饱和土的应力-应变行为。现有模型的基本框架是对经典Mod-Cam-Clay模型的扩展,现在根据四个状态变量进行定义:净平均应力p =(sigma 1 + sigma2 + sigma3)/ 3-u a;偏应力,q =(sigma1-sigma 3);基质吸力,s =(ua-uw);和特定体积,v = 1 + e。概述了在解决增量应力应变行为时本构关系整合的分步过程。然后实施计算本构驱动器,以允许对常规三轴压缩(CTC)和三轴压缩(TC)测试进行数值模拟。模拟是从显式和隐式集成技术获得的。计算算法支持在偏应力(p:q:theta:s)应力平面中进行数值分析,其中theta(Lode-angle)是第三应力不变式,并且使用混合控制(应力和应变控制)本构驱动器结合恒吸方案中的广义凸轮-粘土模型。将设计额外的积分水平,以适应考虑矩阵吸力效应的函数的非线性性质。修改了伺服控制的真三轴(立方)测试设备,以在变化的矩阵吸力条件下测试每侧10.0厘米(4.0英寸)的立方压实非饱和土壤标本。按照多阶段测试方案,通过控制主要,中间和次要主应力,对皮埃蒙特残余土壤的压实粉砂(SM)标本进行了测试。通过使用轴平移技术,在真正的三轴测试过程中可以诱导并保持样品中的基质吸力状态恒定。一系列排水,受应力/吸力控制的CTC和TC测试的结果用于验证在轴对称荷载条件下为非饱和土提出的本构模型,以及在本工作中提出的模型增强。在所有情况下,初始临界状态条件都定义为总剪切应变的约12%。压实粉砂(SM)中观察到的结果与计算结果之间的一致性令人鼓舞,这表明可以将这些模型并入基于FEM的边界值问题分析中,该分析涉及因环境变化而导致负孔隙水压发生显着变化的土壤条件。;在三次方测试设置中进行的一系列排水,应力/吸力控制的三轴压缩(TC),三轴延伸(TE)和简单剪切(SS)测试的真实三轴测试数据用于评估主要钻探的性质。 ,在变化的基质吸力条件下,对于在常规圆柱设备中无法实现的剪切应力路径,每侧立方再压实粉质砂岩(SM)标本的每边10.0厘米(4.0英寸)的次要和中等和中等主应变响应。基质吸力对八面体(sigma1-ua:sigma2-ua:sigma3 ua)和本金(sigma 1-ua:2(sigma2-ua):2(sigma3--)的破坏包络的形状,大小和位置的影响ua))还从真实的三轴测试数据中分析了应力平面。

著录项

  • 作者

    Hoyos, Laureano R., Jr.;

  • 作者单位

    Georgia Institute of Technology.;

  • 授予单位 Georgia Institute of Technology.;
  • 学科 Engineering Civil.; Applied Mechanics.; Engineering Environmental.
  • 学位 Ph.D.
  • 年度 1998
  • 页码 352 p.
  • 总页数 352
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 建筑科学;应用力学;环境污染及其防治;
  • 关键词

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