首页> 外文期刊>Journal of geotechnical and geoenvironmental engineering >Discussion of 'Elastoplastic Deformation Characteristics of Gravelly Soils' by Meng-Chia Weng, Bin-Lin Chu, and Yu-Ling Ho
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Discussion of 'Elastoplastic Deformation Characteristics of Gravelly Soils' by Meng-Chia Weng, Bin-Lin Chu, and Yu-Ling Ho

机译:翁梦佳,朱斌林,何玉玲讨论“砾石土的弹塑性变形特征”

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摘要

The authors are commended for exploring the elastoplastic deformation behavior of gravelly soils though a series of large-scale triaxial compression tests. They concluded that (1) the elastic shear modulus increases with increasing hydrostatic pressure, (2) the influence of confining pressure on plastic deformation is insignificant, (3) gravelly soils follow the nonassociated flow rule, and (4) the plastic potential surface contains an approximate horizontal line and an elliptical surface. The discussers agree with these conclusions except for the second conclusion. Granular soil may show volumetric expansion at a smaller confining pressure and it may present volumetric contraction behavior at a higher confining pressure because of high particle breakage. Therefore, the confining pressure may lead to a variation in the deformation style (i.e., expansion or contraction) of granular soils.
机译:通过一系列大型三轴压缩试验探索了砾石土的弹塑性变形行为受到了作者的赞赏。他们得出的结论是:(1)弹性剪切模量随静水压力的增加而增加;(2)围压对塑性变形的影响微不足道;(3)砾石土遵循非缔合流动规律;(4)塑性势面包含近似的水平线和椭圆表面。讨论者同意这些结论,但第二个结论除外。粒状土壤可能在较小的围压下显示出体积膨胀,并且由于较高的颗粒破裂而在较高的围压下可能表现出体积收缩行为。因此,围压可能导致粒状土壤的变形方式(即膨胀或收缩)变化。

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  • 来源
    《Journal of geotechnical and geoenvironmental engineering》 |2014年第5期|07014007.1-07014007.3|共3页
  • 作者单位

    College of Civil and Transportation Engineering, Hohai Univ., Nanjing 210098, China;

    State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu Univ. of Technology, Chengdu, Sichuan 610051, China and College of Environment and Civil Engineering, Chengdu Univ. of Technology, Chengdu, Sichuan 610051, China;

    School of Civil Engineering, Nanjing Institute of Technology, Nanjing 211167, China;

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  • 入库时间 2022-08-18 00:48:36

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