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Variable density flow in porous media. A study by means of pore level numerical simulations
Author(s) -
Bouhouch A.,
Prat M.,
Boisson H.
Publication year - 1999
Publication title -
international journal for numerical methods in fluids
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.938
H-Index - 112
eISSN - 1097-0363
pISSN - 0271-2091
DOI - 10.1002/(sici)1097-0363(19990730)30:6<725::aid-fld860>3.0.co;2-g
Subject(s) - porous medium , flow (mathematics) , mach number , mechanics , isothermal flow , compressible flow , ideal gas , darcy's law , compressibility , reynolds number , hele shaw flow , mathematics , transient (computer programming) , calculus (dental) , physics , porosity , geology , open channel flow , computer science , geotechnical engineering , turbulence , medicine , dentistry , operating system
This paper is devoted to the modelling of isothermal low Reynolds and Mach numbers transient compressible flow through porous media. Traditionally, this type of flow at the macroscopic level is described by the classical Darcy's law combined with a mass balance that includes the transient term. This model is called the ‘classic model’. The aim of this paper is to explore the validity of this classic model. To this end, the flow of an ideal gas is considered within two‐dimensional model porous media. The flow is due to the imposed pressure variations at the outlet of the fluid domain. At the microscopic level, the flow is computed by solving the full compressible Navier–Stokes equations in two dimensions. Special attention is given to the outlet boundary conditions. The analysis is based on the comparison between the macroscopic data, obtained on the one hand by spatially averaging the microscopic results, and on the other hand by solving the problem directly at the macroscopic level. Situations for which a good agreement is found between the two series of data and situations for which discrepancies are observed are exhibited. These various behaviours are discussed in terms of the various time scales controlling the flow and are explained by analysing the flow structure at pore level. Copyright © 1999 John Wiley & Sons, Ltd.