A general thermodynamical model for finitely-strained continuum with inelasticity and diffusion, its GENERIC derivation in Eulerian formulation, and some application

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Hauptverfasser: Mielke, Alexander, Roubíček, Tomáš
Format: Preprint
Veröffentlicht: 2024
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author Mielke, Alexander
Roubíček, Tomáš
author_facet Mielke, Alexander
Roubíček, Tomáš
contents A thermodynamically consistent visco-elastodynamical model at finite strains is derived that also allows for inelasticity (like plasticity or creep), thermal coupling, and poroelasticity with diffusion. The theory is developed in the Eulerian framework and is shown to be consistent with the thermodynamic framework given by General Equation for Non-Equilibrium Reversible-Irreversible Coupling (GENERIC). For the latter we use that the transport terms are given in terms of Lie derivatives. Application is illustrated by two examples, namely volumetric phase transitions with dehydration in rocks and martensitic phase transitions in shape-memory alloys. A strategy towards a rigorous mathematical analysis is only very briefly outlined.
format Preprint
id arxiv_https___arxiv_org_abs_2404_10126
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle A general thermodynamical model for finitely-strained continuum with inelasticity and diffusion, its GENERIC derivation in Eulerian formulation, and some application
Mielke, Alexander
Roubíček, Tomáš
Mathematical Physics
35Q74, 74L05, 74F05, 74N25, 76A10, 80A19, 86A99
A thermodynamically consistent visco-elastodynamical model at finite strains is derived that also allows for inelasticity (like plasticity or creep), thermal coupling, and poroelasticity with diffusion. The theory is developed in the Eulerian framework and is shown to be consistent with the thermodynamic framework given by General Equation for Non-Equilibrium Reversible-Irreversible Coupling (GENERIC). For the latter we use that the transport terms are given in terms of Lie derivatives. Application is illustrated by two examples, namely volumetric phase transitions with dehydration in rocks and martensitic phase transitions in shape-memory alloys. A strategy towards a rigorous mathematical analysis is only very briefly outlined.
title A general thermodynamical model for finitely-strained continuum with inelasticity and diffusion, its GENERIC derivation in Eulerian formulation, and some application
topic Mathematical Physics
35Q74, 74L05, 74F05, 74N25, 76A10, 80A19, 86A99
url https://arxiv.org/abs/2404.10126