胀

Traditional stress dilatancy theory had been extensively used in constitutive modeling, and its application to clay was very successful.

经典的应力剪胀理论被广泛应用于土体弹塑性本构模型的建立，较好地模拟了黏性土的变形特性。

It is shown that the model in this paper can be included in the nonlinear and dilatancy properties, and the effects of different consolidation pressure and the second main stress.

该模型能同时考虑土体的非线性和剪胀性，以及不同固结压力和第二主应力对地基土的影响。

Illegible knowledge on dilatancy angle has existed for a long time, which caused large errors in theoretical analysis and numerical simulation.

当前对剪胀角存在模糊认识，导致在理论分析和数值模拟分析中常会产生较大误差。

The modified Rowe's dilatancy equation will be more adaptive to the unsliding deformation of particles.

修正Rowe剪胀方程对颗粒非滑移变形具有更好的适应性。

The results show that this decoupling method can predict the evolvements of pore water pressure and settlement, and reflect the effect of stress path and dilatancy.

证明了该解耦方法的能较好预测孔压以及沉降的变化，并在分析过程中能较好反映应力路径及剪胀性等特性的影响。

The so called state-dependent dilatancy theory was suggested and applied in sand modeling.

本文就砂土的状态及其描述、剪胀理论的发展、砂土本构模拟等方面进行介绍。

The aqueous solution of WSPs shows a weak feature of dilatancy fluid.

水溶性聚酯水溶液表现出微弱的胀塑性流体特征。

A modified model combining the theory of state-dependent dilatancy with thermodynamics laws is proposed.

考虑剪胀对砂土内部状态的依赖，建立了统一的弹塑性本构模型以描述具有不同密度和应力水平的砂的变形特性。

The volumetric strain due to stress-dilatancy of sand is found to be composed of a reversible dilatancy component and an irreversible dilatancy component.

基于对较高精度的砂土扭剪试验成果的分析，表明砂土的剪胀是由一个完全可逆的体应变分量和一个不可逆的体应变分量构成的。

A lateral deformation coefficient was used in analyzing this type of composite ground with dilatant materials, and this method provides a new available way to solve this kind of problem.

将碎石料看作不完全弹性材料，引入横向变形系数，对碎石复合体进行了理论分析和数值计算，本方法为解决计算包含剪胀材料的散体桩复合地基的应力和变形这一焦点问题提供了新的思路。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。