代志宏, 吴恒, 张信贵. 2004: 附加应力在土体中传递分布的细观模型. 工程地质学报, 12(S1): 73-78.
    引用本文: 代志宏, 吴恒, 张信贵. 2004: 附加应力在土体中传递分布的细观模型. 工程地质学报, 12(S1): 73-78.
    DAI Zhihong, WU Heng, ZHANG Xingui. 2004: THE MESOSCOPIC STRUCTURE MODEL OF ADDITIONAL STRESS TRANSFER IN THE SOIL. JOURNAL OF ENGINEERING GEOLOGY, 12(S1): 73-78.
    Citation: DAI Zhihong, WU Heng, ZHANG Xingui. 2004: THE MESOSCOPIC STRUCTURE MODEL OF ADDITIONAL STRESS TRANSFER IN THE SOIL. JOURNAL OF ENGINEERING GEOLOGY, 12(S1): 73-78.

    附加应力在土体中传递分布的细观模型

    THE MESOSCOPIC STRUCTURE MODEL OF ADDITIONAL STRESS TRANSFER IN THE SOIL

    • 摘要: 地基土体中,附加应力的研究一直建立在弹性连续介质假设的基础上。但土体是固、液、气三相组成的松散体系,土体结构是由许多个层次组成的复杂系统,它与弹性连续介质相差甚远。为了更准确的反映附加应力的基本规律,本文将从细观结构角度着手,建立应力传递分布的细观模型,研究其产生机理、演化规律,并利用所建模型成功的解释了成层地基中附加应力的集中、扩散现象。

       

      Abstract: In the previous study on additional stress in soil of ground always, soil is apt to be assumed as an elastic continuous medium. In fact, since soil is a solid-liquid-gas three-phase incompact system and the structure of soil is a complex system formed by several levels, it is greatly different from elastic continuous medium. To represent regularity of additional stress more correctly, the mesoscopic structure model of additional stress transfer in the soil is proposed to study its mechanics in this paper. This model also explains concentration and diffusion of additional stress in layered ground.

       

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