TY - GEN
T1 - A stability condition for the numerical simulation of poroelastic systems
AU - Favino, Marco
AU - Grillo, Alfio
AU - Krause, Rolf
PY - 2013
Y1 - 2013
N2 - In the numerical simulation of the Biot model numerical oscillations may occur if the spatial and discretization parameters are not properly chosen. When the time-step is too small, the grid has to be fine enough to resolve the boundary layers that appear in the early stages of the simulation. In this work, we extend a strategy that has been successfully employed in the one-dimensional case for the detection of a critical time-step, below which instabilities appear. The idea is to study under which condition the Schur complement of the poroelastic system enjoys a discrete maximum principle property. Differently from the one-dimensional case, in the vectorial case the shear modulus plays a fundamental role for the computation of the Schur complement and the maximum principle argument can be applied only for small shear. We will also investigate the sign of the entries of the Schur complement when the shear and the bulk modulus are of the same magnitude.
AB - In the numerical simulation of the Biot model numerical oscillations may occur if the spatial and discretization parameters are not properly chosen. When the time-step is too small, the grid has to be fine enough to resolve the boundary layers that appear in the early stages of the simulation. In this work, we extend a strategy that has been successfully employed in the one-dimensional case for the detection of a critical time-step, below which instabilities appear. The idea is to study under which condition the Schur complement of the poroelastic system enjoys a discrete maximum principle property. Differently from the one-dimensional case, in the vectorial case the shear modulus plays a fundamental role for the computation of the Schur complement and the maximum principle argument can be applied only for small shear. We will also investigate the sign of the entries of the Schur complement when the shear and the bulk modulus are of the same magnitude.
UR - http://www.scopus.com/inward/record.url?scp=84887397857&partnerID=8YFLogxK
U2 - 10.1061/9780784412992.110
DO - 10.1061/9780784412992.110
M3 - Conference contribution
AN - SCOPUS:84887397857
SN - 9780784412992
T3 - Poromechanics V - Proceedings of the 5th Biot Conference on Poromechanics
SP - 919
EP - 928
BT - Poromechanics V - Proceedings of the 5th Biot Conference on Poromechanics
T2 - 5th Biot Conference on Poromechanics, BIOT 2013
Y2 - 10 July 2013 through 12 July 2013
ER -