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基于对数应变的孔隙黏弹性有限变形理论

Finite Deformation Theory of Poroviscoelasticity Based on Logarithmic Strain
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摘要 在有限变形理论框架下,基于对数应变和Kelvin流变模型提出一个孔隙黏弹性理论模型。该模型通过假设Kirchhoff应力和孔隙压力与对数应变和Lagrangian孔隙度的变化量存在线性关系,将线性孔隙黏弹性模型中的无穷小应变直接替换为对数应变而得到。作为验证,将该理论模型用于研究经典的Terzaghi一维固结问题,通过与孔隙弹性有限变形模型的数值结果对比,结果显示:在固结早期,孔隙固体骨架的黏弹性响应和弹性响应曲线几乎是一致的,但随着时间的推移,孔隙固体骨架的黏性逐渐主导骨架的变形,并影响固结的最终结果;并且,骨架的黏性会延迟孔隙压力的扩散。此外,通过设置黏性贡献系数ζ=0.001,从数值角度实现了孔隙黏弹性响应“退化”为孔隙弹性响应,这在一定程度上验证了模型的正确性。 In the framework of finite deformation theory,a theoretical model of poroviscoelasticity is proposed which is based on logarithmic strain and Kelvin rheological model.The model is obtained by assuming a linear relationship between Kirchhoff stress and pore pressure and logarithmic strain and the variation of Lagrangian porosity,and then directly replacing the infinitesimal strain in the linear pore viscoelastic model with the logarithmic strain.As a verification,the theoretical model is used to study the classic Terzaghi’s one-dimensional consolidation problem.By comparing with the numerical results of the poroelastic finite deformation model,the results show that the viscoelastic response and elastic response curves of the pore solid skeleton are almost identical in the early stage of consolidation,but with the passage of time,the viscous response of the pore solid skeleton gradually dominates the deformation of the skeleton and affects the final result of consolidation.In addition,the viscous response of the skeleton delays the diffusion of pore pressure.In addition,by setting the viscosity contribution coefficientζ=0.001,the poroviscoelastic response is numerically“degraded”to the poroelastic response,which verifies the correctness of the model to a certain extent.
作者 唐熊 郑佩 TANG Xiong;ZHENG Pei(School of Mechanical Engineering,University of Shanghai for Science and Technology,Shanghai 200093,China)
出处 《计算物理》 CSCD 北大核心 2024年第3期287-297,共11页 Chinese Journal of Computational Physics
关键词 孔隙黏弹性 对数应变 有限变形 有限元 流变模型 poroviscoelasticity logarithmic strain finite deformation finite elements rheological model
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