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arXiv 2103.02560cond-mat.softphysics.flu-dyn
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非线性Maxwell-Oldroyd型模型在简单剪切作用下的中幅响应

The Medium Amplitude Response of Nonlinear Maxwell-Oldroyd Type Models in Simple Shear

Kyle R. Lennon, Gareth H. McKinley, James W. Swan

摘要:

Maxwell-Oldroyd型微分本构模型的一般框架进行检查,其中未指定的非线性函数的应力和变形率张量被纳入著名的共旋版本的Jeffreys模型讨论的Oldroyd。对于中等振幅的简单剪切变形,最近开发的数学框架的中等振幅平行叠加(MAPS)流变学表明,这种广义的非线性麦克斯韦模型只能产生有限数量的不同的签名,线性组合在一个适定的基础上展开的三阶复数粘度。该基础展开表示包含在广义非线性Maxwell模型内的不同本构模型的MAPS签名库。我们描述了一个框架,定量模型识别使用此基础扩展,并讨论其局限性,区分不同的非线性特征的基础本构模型从中等振幅剪切应力数据。还考虑了正应力差的首阶贡献,揭示了只有第二正应力差提供了关于模型的弱非线性响应空间的独特信息。在简要考虑广义非线性Maxwell模型的时间-应变可分离性的条件后,我们应用三阶复粘性的基展开来推导该模型在特定剪切变形协议中的介质振幅特征。最后,我们使用这些签名从这些不同的变形协议获得的流变数据的模型参数的估计,揭示三音振荡剪切变形产生的数据,是很容易能够区分所有功能的介质振幅,简单的剪切响应空间的本构模型的广义类。

英文摘要:

A general framework for Maxwell-Oldroyd type differential constitutive models is examined, in which an unspecified nonlinear function of the stress and rate-of-deformation tensors is incorporated into the well-known corotational version of the Jeffreys model discussed by Oldroyd. For medium amplitude simple shear deformations, the recently developed mathematical framework of medium amplitude parallel superposition (MAPS) rheology reveals that this generalized nonlinear Maxwell model can produce only a limited number of distinct signatures, which combine linearly in a well-posed basis expansion for the third order complex viscosity. This basis expansion represents a library of MAPS signatures for distinct constitutive models that are contained within the generalized nonlinear Maxwell model. We describe a framework for quantitative model identification using this basis expansion, and discuss its limitations in distinguishing distinct nonlinear features of the underlying constitutive models from medium amplitude shear stress data. The leading order contributions to the normal stress differences are also considered, revealing that only the second normal stress difference provides distinct information about the weakly nonlinear response space of the model. After briefly considering the conditions for time-strain separability within the generalized nonlinear Maxwell model, we apply the basis expansion of the third order complex viscosity to derive the medium amplitude signatures of the model in specific shear deformation protocols. Finally, we use these signatures for estimation of model parameters from rheological data obtained by these different deformation protocols, revealing that three-tone oscillatory shear deformations produce data that is readily able to distinguish all features of the medium amplitude, simple shear response space of this generalized class of constitutive models.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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