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Shrinkage cracking of soils and cementitiously-stabilized soils: Mechanisms and modeling.

机译:土壤和胶结稳定土的收缩开裂:机理和模型。

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摘要

Shrinkage cracking of soil or cement soil can cause the infiltration or seepage of water into the material and lead to reflective cracking in the structure above it. Shrinkage cracking greatly limits the use of cementitious stabilization. Drying shrinkage is the major problem associated with shrinkage cracking. Although some studies on the drying shrinkage cracking of concrete have been carried out, few research efforts have focused on unsaturated soil and cement soil. Even fewer studies consider the shrinkage stress distribution and evolution of the stress profile during drying and/or cement hydration in shrinkage cracking modeling.;Using two types of soil and two types of cement soil, this study investigates the soil and cement soil properties that are related to drying shrinkage and shrinkage cracking. These material properties, which are considered in this study to be dependent on pore relative humidity (RH) and/or cement hydration and, therefore, are neither uniform nor constant during drying and/or cement hydration, include the humidity isotherm, diffusion coefficient, soil water characteristic curve (SWCC), tensile strength, tensile stress-strain relationship, and shrinkage potential, etc. This study examines the effects of pore RH and/or cement hydration on these material properties. Models are developed herein to predict the evolution of these material properties during drying and/or cement hydration.;By measuring the humidity isotherm and diffusion coefficient and using the finite element (FE) method, the evolution of the pore RH gradient within the soil or cement soil specimens during drying can be fully captured. A coefficient of moisture shrinkage is proposed to bridge the knowledge gap between pore RH and shrinkage potential, which is defined in this study as the maximum possible drying shrinkage of a material at a given pore RH when there is no restraint. Then, the pore RH and/or cement hydration-dependent tensile strength, tensile stress-strain relationship, and shrinkage potential within the specimens during drying and/or cement hydration can be fully understood using the models developed in this study. Finally, FE modeling case studies were conducted to verify the models and procedure proposed in this study to predict shrinkage stress and shrinkage cracking. The results were compared with results from laboratory experiments and good agreement was found.
机译:土壤或水泥土的收缩开裂会导致水渗入或渗入材料,并导致其上方结构发生反射性开裂。收缩开裂极大地限制了水泥稳定剂的使用。干燥收缩是与收缩开裂有关的主要问题。尽管已经对混凝土的干燥收缩开裂进行了一些研究,但很少有研究工作集中在非饱和土和水泥土上。甚至更少的研究在收缩裂缝建模中考虑干燥和/或水泥水化过程中的收缩应力分布和应力分布的演变。使用两种土壤和两种水泥土壤,本研究调查了土壤和水泥土的特性。与干燥收缩和收缩开裂有关。这些材料特性在本研究中被认为取决于孔隙相对湿度(RH)和/或水泥水化,因此在干燥和/或水泥水化过程中既不均匀也不恒定,包括湿度等温线,扩散系数,土壤水分特征曲线(SWCC),抗张强度,张应力-应变关系和收缩势等。这项研究研究了孔隙RH和/或水泥水化对这些材料特性的影响。本文开发了模型来预测干燥和/或水泥水化过程中这些材料特性的演变。通过测量湿度等温线和扩散系数并使用有限元(FE)方法,土壤或土壤中孔隙RH梯度的演变干燥期间的水泥土标本可以被完全捕获。提出了一种水分收缩系数来弥合孔隙RH和收缩潜力之间的知识鸿沟,在本研究中定义为在没有约束的情况下,在给定的孔隙RH下,材料在最大干燥收缩率。然后,通过使用本研究开发的模型,可以充分了解孔相对湿度和/或水泥水化的拉伸强度,拉伸应力-应变关系以及试样在干燥和/或水泥水化过程中的收缩潜力。最后,进行有限元建模案例研究以验证本研究中提出的预测收缩应力和收缩裂纹的模型和程序。将该结果与实验室实验的结果进行比较,发现吻合良好。

著录项

  • 作者

    Li, Xiaojun.;

  • 作者单位

    Washington State University.;

  • 授予单位 Washington State University.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2014
  • 页码 200 p.
  • 总页数 200
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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