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无状态变量的状态依赖剪胀方程及其本构模型
引用本文:孙逸飞,陈成.无状态变量的状态依赖剪胀方程及其本构模型[J].岩土力学,2019,40(5):1813-1822.
作者姓名:孙逸飞  陈成
作者单位:1. 河海大学 岩土力学与堤坝工程教育部重点实验室,江苏 南京 210098; 2. 武汉理工大学 土木工程与建筑学院,湖北 武汉 430070
基金项目:中央高校基本科研业务费(No. 2017B05214);博士后面上基金项目(No. 2017M621607)。
摘    要:粗粒土的剪胀行为具有状态依赖特性。为了考虑这一特性,不同的状态依赖变量被唯像地提出,并被经验性地内嵌入已有剑桥、修正剑桥等剪胀方程中。基于分数阶梯度律,用理论推导出了分数阶状态依赖剪胀方程,并阐述了分数阶数的物理意义。所得剪胀比大小受3个因素影响:分数阶求导阶数、当前加载应力以及当前应力到临界状态应力的距离。当分数阶求导阶数从1开始增大时,分数阶剪胀曲线自修正剑桥剪胀曲线向剑桥剪胀曲线移动;而当求导阶数从1开始减小时,分数阶剪胀曲线逐渐远离修正剑桥剪胀曲线;当求导阶数等于1时,分数阶剪胀曲线与修正剑桥剪胀曲线重合。为验证所提出的状态依赖剪胀方程,基于该方程进一步建立了砂土的状态依赖分数阶塑性力学本构模型,并对砂土和堆石料的三轴排水与不排水试验结果进行了模拟。研究表明,基于状态依赖分数阶剪胀方程建立的本构模型,可以合理地描述砂土在不同初始状态及加载条件下的应力-应变行为。与砂土UH模型预测结果对比发现,UH模型预测较好。

关 键 词:分数阶微分  塑性力学  本构模型  状态依赖  砂土  
收稿时间:2018-01-12

A state-dependent stress-dilatancy equation without state index and its associated constitutive model
SUN Yi-fei,CHEN Cheng.A state-dependent stress-dilatancy equation without state index and its associated constitutive model[J].Rock and Soil Mechanics,2019,40(5):1813-1822.
Authors:SUN Yi-fei  CHEN Cheng
Institution:1. Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, Jiangsu 210098; 2. School of Civil Engineering and Architecture, Wuhan University of Technology, Wuhan, Hubei 430070
Abstract:It has been recognized that the stress-dilatancy behaviour of granular soil depends on its material state. To consider such state-dependence, a variety of state parameters were suggested phenomenologically and incorporated into existing stress-dilatancy equations, e.g. Cam-clay equation, modified Cam-clay equation, by experience. In this study, a novel state-dependent stress-dilatancy equation is developed by using fractional stress gradient, where physical meaning of the fractional order is provided. The obtained stress-dilatancy ratio is determined by three factors: the fractional order, current load stress, and the distance from current stress to critical state stress. When the fractional order is larger than 1, the stress-dilatancy curve shifts from the modified Cam-clay stress-dilatancy curve towards the Cam-clay stress-dilatancy curve. However, when the fractional order is smaller than 1, the stress-dilatancy curve is located above the modified Cam-clay stress-dilatancy curve. When the fractional order is equal to 1, the proposed stress-dilatancy curve coincides with the modified Cam-clay curve. To validate the proposed approach, a state-dependent fractional plasticity model for sand soils is established by using the proposed stress-dilatancy equation. Then, a series of drained and undrained triaxial compression tests on sand and rockfill with different initial states is simulated and compared, from which a good agreement between the model simulations and the corresponding test results can be observed. Comparison with the model predictions of the UH sand model indicates that the UH model gives better prediction.
Keywords:fractional calculus  plasticity  constitutive model  state dependence  sand  
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