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Stress-dilatancy Relation for Mohr-Coulomb Soils Following a Non-Associated Flow Rule

机译:遵循非关联流规则的摩尔库仑土的应力-剪胀关系

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摘要

Roweu27s stress–dilatancy relation for frictional (cohesionless) materials has been a cornerstone of soil mechanics. The original derivation of this relationship was based on incorrect energy minimisation considerations, but the relationship was proven later by De Josselin de Jong using friction laws, and has been confirmed by a large body of experimental results. In contrast, the validity of Roweu27s stress–dilatancy relation for cohesive-frictional materials, which has also been used, although not as extensively, was never verified. This paper shows that Roweu27s stress–dilatancy relation for Mohr–Coulomb soils (cohesive-frictional materials) is in fact incorrect. The paper also provides a correct stress–dilatancy relationship for non-associated Mohr–Coulomb soils that have both cohesive and frictional strength components. The derivation of the relationship for cohesive-frictional soils presented in this paper relies on use of the sawtooth model together with the application of the laws of friction.
机译:Rowe对摩擦(无粘性)材料的应力-剪胀关系一直是土壤力学的基石。这种关系的原始推导是基于不正确的能量最小化考虑,但后来由De Josselin de Jong使用摩擦定律证明了这种关系,并已得到大量实验结果的证实。相反,Rowe应力-剪胀关系对于粘滞摩擦材料的有效性(尽管没有得到广泛应用)也从未得到验证。本文表明,Rowe的Mohr-Coulomb土(粘性摩擦材料)的应力-剪胀关系实际上是不正确的。本文还为具有黏结强度和摩擦强度成分的非缔合莫尔-库仑土壤提供了正确的应力-剪胀关系。本文提出的粘性摩擦土的关系的推导依赖于锯齿模型的应用以及摩擦定律的应用。

著录项

  • 作者

    Zhang J; Salgado Rodrigo;

  • 作者单位
  • 年度 2010
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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