Sciact
  • EN
  • RU

Numerical Solution of Anisotropic Biot Equations in Quasi-static State Full article

Journal Lecture Notes in Computer Science
ISSN: 0302-9743 , E-ISSN: 1611-3349
Output data Year: 2022, Volume: 13378 LNCS, Pages: 310-327 Pages count : 18 DOI: 10.1007/978-3-031-10562-3_23
Tags Direct methods for SLAE; Finite differences; Poroelaticity; Quasi-static state; Wave-induced fluid flow
Authors Solovyev S. 1 , Novikov M. 2 , Lisitsa V. 1
Affiliations
1 Institute of Mathematics SB RAS, Koptug ave. 4, Novosibirsk, 630090, Russian Federation
2 Institute of Petroleum Geology and Geophysics SB RAS, Koptug ave. 3, Novosibirsk, 630090, Russian Federation

Funding (1)

1 Russian Science Foundation 19-77-20004

Abstract: Frequency-dependent seismic attenuation can be applied to indicate transport properties of fractured media and fluid mobility within it. In particular, wave-induced fluid flow (WIFF) appears during seismic wave propagation between fractures and background as well as within interconnected fractures, and causes intensive attenuation. We present effective algorithm for numerical upscaling to estimate attenuation in anisotropic fractured porous fluid-saturated media. Algorithm is based on numerical solution of quasi-static Biot equations using finite-difference approximation. Presented algorithm is used to estimate seismic attenuation in fractured media with high fracture connectivity. Results of numerical experiments demonstrate the influence of physical properties and microscale anisotropy of fracture-filling material on seismic attenuation.
Cite: Solovyev S. , Novikov M. , Lisitsa V.
Numerical Solution of Anisotropic Biot Equations in Quasi-static State
Lecture Notes in Computer Science. 2022. V.13378 LNCS. P.310-327. DOI: 10.1007/978-3-031-10562-3_23 Scopus OpenAlex
Dates:
Published online: Aug 4, 2022
Identifiers:
Scopus: 2-s2.0-85135926505
OpenAlex: W4289601188
Citing:
DB Citing
Scopus 1
OpenAlex 5
Altmetrics: