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Recognition of the Stress-Strain Curve Based on the Local Deformation Measurement of Soil Specimens in the Triaxial Test

机译:三轴试验中基于土样局部变形测量的应力应变曲线识别

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摘要

A digital image technique was developed and used to measure the deformation distribution over the entire surface of soil specimens in triaxial tests. The measured deformation process shows that the specimen apparently exhibits three states during the test, i.e., pre-failure, in-failure, and post-failure, in correspondence to the different features of its deformation. The deformation feature in each state is then analyzed by the displacement and strain contours. Additionally, the stress level, S, is calculated to determine whether the soil is in failure at a point (representative element volume (REV)) on the surface of the specimen. Next, the failure zone, namely the shear band, was considered to be enveloped by the curve defined by S = 1 on the stress-level contour map. The stress level is calculated based on the strain, Young's modulus and Poisson's ratio. According to analysis of the deformation feature and the failure process, we recognized the following properties: (i) the deformation of the specimen was approximately uniform in the pre-failure state; (ii) failure occurred from a point and developed gradually until the shear band cleaves the specimen; (iii) in the post-failure state, deformation was exclusively due to the blocks of the specimen sliding along the shear band; (iv) the deformation feature in the shear band was quite different from that outside the shear band. In conclusion, the stress-strain curve of the specimen revealed a structural response, not an elementary response, especially in the in-failure and post-failure states, in which the deformation features of different corner points were different, and the observed deformation for the entire specimen may be the combination of local deformations. Therefore, it is not appropriate to build the constitutive model for soil according to the stress-strain curves of the entire deformation process and to take the specimen as a uniform element in the entire process.
机译:开发了一种数字图像技术,并用于在三轴测试中测量土样整个表面的变形分布。测得的变形过程表明,试样在测试过程中显然表现出三种状态,即失效前,失效内和失效后三种状态,分别对应于其变形的不同特征。然后,通过位移和应变轮廓分析每种状态下的变形特征。另外,计算应力水平S,以确定土壤是否在试样表面的某个点(代表元素体积(REV))处破裂。接下来,破坏区域,即剪切带,被认为被应力水平轮廓图上S = 1定义的曲线所包围。根据应变,杨氏模量和泊松比计算应力水平。通过对变形特征和破坏过程的分析,我们认识到以下特性:(i)在破坏前的状态下,试样的变形大致均匀; (ii)从某一点开始发生破坏,并逐渐发展直至剪切带将试样劈裂; (iii)在破坏后的状态下,变形完全是由于试样块沿着剪切带滑动引起的; (iv)剪切带内的变形特征与剪切带外的特征完全不同。总之,试样的应力-应变曲线显示出结构响应,而不是基本响应,特别是在失效和失效后状态下,其中不同角点的变形特征不同,并且观察到的变形整个样本可能是局部变形的组合。因此,不宜根据整个变形过程的应力-应变曲线建立土的本构模型,并在整个过程中将试样作为统一元素。

著录项

  • 来源
    《Geotechnical testing journal》 |2016年第4期|658-672|共15页
  • 作者单位

    Dalian Univ Technol, Dept Engn Mech, State Key Lab Struct Anal Ind Equipment, Room 308, Dalian 116024, Liaoning Provin, Peoples R China|Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Liaoning Provin, Peoples R China;

    Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Liaoning Provin, Peoples R China|Dalian Univ Technol, Dept Engn Mech, Dalian 116024, Liaoning, Peoples R China;

    Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Liaoning Provin, Peoples R China|Dalian Univ Technol, Dept Engn Mech, Dalian 116024, Liaoning, Peoples R China;

    Dalian Univ Technol, State Key Lab Struct Anal Ind Equipment, Dalian 116024, Liaoning Provin, Peoples R China|Dalian Univ Technol, Dept Engn Mech, Dalian 116024, Liaoning, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    local deformation measurement; deformation distribution; stress level; stress-strain curve;

    机译:局部变形测量变形分布应力水平应力应变曲线;

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