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EQUATIONS OF STATE IN SOIL COMPRESSION BASED ON STATISTICAL MECHANICS

机译:基于统计力学的土壤压缩状态方程

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References(34) Cited-By(1) There have been many theories and interpretations of the compression process for soil. However due to the complexity of the compression process for a wide range of soil states, i.e., suspended, liquid, plastic, semisolid or solid states like rock, the interaction between the states or the transition from one state to another, there have often been misunderstandings and difficulties regarding the application of these theories. In this study, an ideal particle distribution in an ideal ground system is derived to find the equation of state, a general compression process for a wide variety of soil types and states. In other words, it is a general relationship between the void ratio and effective overburden pressure in terms of interparticle energy and is thus a “law of soil.” The principle is based on the law of energy distribution in statistical mechanics. The derived equations can be applied to describe the void ratio profile and the compression process of various soils. Case studies show that this theoretical approach agrees well with the experimental data obtained for several soils such as sediments, Mexican City clay, sand and others.
机译:参考文献(34)Cited-By(1)有许多关于土壤压缩过程的理论和解释。但是,由于压缩过程对于多种土壤状态(例如,岩石的悬浮状态,液体状态,塑料状态,半固态状态或固态状态)的复杂性,状态之间的相互作用或从一种状态到另一种状态的转换经常会发生这些理论的应用存在误解和困难。在这项研究中,推导了理想地面系统中的理想颗粒分布,以找到状态方程,这是针对各种土壤类型和状态的一般压缩过程。换句话说,它是空隙率与有效覆盖层压力之间的一般关系,以粒子间能量而言,因此是“土壤定律”。该原理基于统计力学中的能量分布定律。导出的方程可用于描述孔隙率分布和各种土壤的压缩过程。案例研究表明,这种理论方法与从几种土壤(例如沉积物,墨西哥城粘土,沙子等)获得的实验数据非常吻合。

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