Bounding surface plasticity for sand using fractional flow rule and modified critical state line

被引:10
作者
Sun, Yifei [1 ,2 ]
Sumelka, Wojciech [3 ]
Gao, Yufeng [4 ]
机构
[1] Hohai Univ, Minist Educ Geomech & Embankment Engn, Key Lab, Nanjing 210098, Peoples R China
[2] Ruhr Univ Bochum, Fac Civil & Environm Engn, D-44801 Bochum, Germany
[3] Poznan Univ Tech, Inst Struct Anal, Piotrowo 5, PL-60965 Poznan, Poland
[4] Hohai Univ, Coll Civil & Transportat Engn, Minist Educ Geomech & Embankment Engn, Key Lab, Nanjing 210098, Peoples R China
基金
中国国家自然科学基金;
关键词
Fractional order; Critical state; State dependence; Constitutive relation; Sand; ELASTOPLASTIC CONSTITUTIVE MODEL; GENERALIZED PLASTICITY; SOILS; BEHAVIOR; STRESS; PARAMETER;
D O I
10.1007/s00419-020-01737-9
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Bounding surface plasticity has been widely used for capturing the stress-strain behaviour of geomaterials. However, it may require multiple sets of model parameters for constitutive modelling of sands with a wide range of initial states, because of the distinct critical state characteristics under low and high densities or pressures in the e - In p' plane. In this study, an enhanced bounding surface plasticity approach for sand with a wide range of initial material states is developed. A fractional plastic flow rule and a modified critical state line are suggested, which ensures that without using any predefined state indices, the developed model can consider the state-dependent dilatancy and hardening behaviours of sand subjected to low and high pressures/densities. The approach is validated by simulating the well-documented test results of Toyoura sand and Sacramento River sand. For comparison, the original state-dependent dilatancy approach in Li and Dafalias (Geotechnique 50(4):449-460, 2000. https://doi.org/10.1680/geot.2000.50.4.449) is also adopted and implemented. It is found that the two approaches can reasonably capture the typical stress-strain behaviour, e.g. hardening/contraction, softening/dilation, liquefaction, quasi-steady state flow, and non-flow, of sands with different initial material states, by using a single set of model parameters. However, compared to the current work, Li and Dafalias (2000) model relied on a predefined state parameter, for capturing the state-dependent behaviour of sand under a wide range of initial states
引用
收藏
页码:2561 / 2577
页数:17
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