Details
Originalsprache | Englisch |
---|---|
Aufsatznummer | 113048 |
Fachzeitschrift | Computer Methods in Applied Mechanics and Engineering |
Jahrgang | 366 |
Frühes Online-Datum | 23 Apr. 2020 |
Publikationsstatus | Veröffentlicht - 1 Juli 2020 |
Abstract
In this paper we study the equations of semi-linear thermoporoelasticity. Starting point is the dimensionless formulation in van Duijn et al. (2019), which was obtained by a formal two-scale expansion. Nonlinearities in the equations arise through the fluid viscosity and the thermal conductivity, both may depend on temperature, and through the coupling in the heat convection by the Darcy discharge in the energy equation. The coupled system of equations involves as unknowns the skeleton displacement, Darcy discharge, fluid pressure and temperature. We treat the system in its incremental (i.e. time-discrete) form. We prove existence by applying a fundamental theorem of Brézis on pseudo-monotone operators. Moreover we show that the free energy of the system acts as a Lyapunov functional. This yields global stability in the time-stepping process. Our theoretical results are substantiated with two-dimensional numerical tests using a monolithic formulation. Temporal discretization is based on the backward Euler scheme and finite elements are employed for the spatial discretization. The semi-linear discrete system is solved with Newton's method. In the proposed numerical examples, different source terms are employed and spatial mesh refinement studies show computational convergence.
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in: Computer Methods in Applied Mechanics and Engineering, Jahrgang 366, 113048, 01.07.2020.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Mathematical theory and simulations of thermoporoelasticity
AU - van Duijn, Cornelis J.
AU - Mikelić, Andro
AU - Wick, Thomas
N1 - Funding information: CJvD acknowledges the support of the Darcy Center (Utrecht University - Eindhoven University of Technology), The Netherlands and of the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) for supporting this work by funding SFB 1313, Project Number327154368.This work of A.M. benefited from the support of the project UPGEO ?ANR-19-CU05-032? of the French National Research Agency (ANR) and from the LABEX MILYON (ANR-10-LABX-0070) of Université de Lyon, within the program ”Investissements d'Avenir” (ANR-11-IDEX-0007) operated by the French National Research Agency (ANR).
PY - 2020/7/1
Y1 - 2020/7/1
N2 - In this paper we study the equations of semi-linear thermoporoelasticity. Starting point is the dimensionless formulation in van Duijn et al. (2019), which was obtained by a formal two-scale expansion. Nonlinearities in the equations arise through the fluid viscosity and the thermal conductivity, both may depend on temperature, and through the coupling in the heat convection by the Darcy discharge in the energy equation. The coupled system of equations involves as unknowns the skeleton displacement, Darcy discharge, fluid pressure and temperature. We treat the system in its incremental (i.e. time-discrete) form. We prove existence by applying a fundamental theorem of Brézis on pseudo-monotone operators. Moreover we show that the free energy of the system acts as a Lyapunov functional. This yields global stability in the time-stepping process. Our theoretical results are substantiated with two-dimensional numerical tests using a monolithic formulation. Temporal discretization is based on the backward Euler scheme and finite elements are employed for the spatial discretization. The semi-linear discrete system is solved with Newton's method. In the proposed numerical examples, different source terms are employed and spatial mesh refinement studies show computational convergence.
AB - In this paper we study the equations of semi-linear thermoporoelasticity. Starting point is the dimensionless formulation in van Duijn et al. (2019), which was obtained by a formal two-scale expansion. Nonlinearities in the equations arise through the fluid viscosity and the thermal conductivity, both may depend on temperature, and through the coupling in the heat convection by the Darcy discharge in the energy equation. The coupled system of equations involves as unknowns the skeleton displacement, Darcy discharge, fluid pressure and temperature. We treat the system in its incremental (i.e. time-discrete) form. We prove existence by applying a fundamental theorem of Brézis on pseudo-monotone operators. Moreover we show that the free energy of the system acts as a Lyapunov functional. This yields global stability in the time-stepping process. Our theoretical results are substantiated with two-dimensional numerical tests using a monolithic formulation. Temporal discretization is based on the backward Euler scheme and finite elements are employed for the spatial discretization. The semi-linear discrete system is solved with Newton's method. In the proposed numerical examples, different source terms are employed and spatial mesh refinement studies show computational convergence.
KW - Free energy and stability
KW - Heat convection by Darcy's velocity
KW - Monolithic numerical scheme
KW - Thermoporoelasticity equations
UR - http://www.scopus.com/inward/record.url?scp=85083668572&partnerID=8YFLogxK
U2 - 10.1016/j.cma.2020.113048
DO - 10.1016/j.cma.2020.113048
M3 - Article
AN - SCOPUS:85083668572
VL - 366
JO - Computer Methods in Applied Mechanics and Engineering
JF - Computer Methods in Applied Mechanics and Engineering
SN - 0045-7825
M1 - 113048
ER -