Homogenized model for flow in partially fractured media
We derive rigorously a homogenized model for the displacement of one compressible miscible fluid by another in a partially fractured porous reservoir. We denote by $epsilon$ the characteristic size of the heterogeneity in the medium. A function $alpha$ characterizes the cracking degree of the...
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Texas State University
2009-01-01
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doaj-824711950bbb4b58a199295e78a6dc262020-11-25T02:28:44ZengTexas State UniversityElectronic Journal of Differential Equations1072-66912009-01-01200901,127Homogenized model for flow in partially fractured mediaCatherine ChoquetWe derive rigorously a homogenized model for the displacement of one compressible miscible fluid by another in a partially fractured porous reservoir. We denote by $epsilon$ the characteristic size of the heterogeneity in the medium. A function $alpha$ characterizes the cracking degree of the rock. Our starting point is an adapted microscopic model which is scaled by appropriate powers of $epsilon$. We then study its limit as $epsilon o 0$. Because of the partially fractured character of the medium, the equation expressing the conservation of total mass in the flow is of degenerate parabolic type. The homogenization process for this equation is thus nonstandard. To overcome this difficulty, we adapt two-scale convergence techniques, convexity arguments and classical compactness tools. The homogenized model contains both single porosity and double porosity characteristics.http://ejde.math.txstate.edu/Volumes/2009/01/abstr.htmlMiscible compressible displacementporous mediumpartially fractured reservoirdouble porosityhomogenizationtwo-scale limit of a degenerate parabolic equation |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Catherine Choquet |
spellingShingle |
Catherine Choquet Homogenized model for flow in partially fractured media Electronic Journal of Differential Equations Miscible compressible displacement porous medium partially fractured reservoir double porosity homogenization two-scale limit of a degenerate parabolic equation |
author_facet |
Catherine Choquet |
author_sort |
Catherine Choquet |
title |
Homogenized model for flow in partially fractured media |
title_short |
Homogenized model for flow in partially fractured media |
title_full |
Homogenized model for flow in partially fractured media |
title_fullStr |
Homogenized model for flow in partially fractured media |
title_full_unstemmed |
Homogenized model for flow in partially fractured media |
title_sort |
homogenized model for flow in partially fractured media |
publisher |
Texas State University |
series |
Electronic Journal of Differential Equations |
issn |
1072-6691 |
publishDate |
2009-01-01 |
description |
We derive rigorously a homogenized model for the displacement of one compressible miscible fluid by another in a partially fractured porous reservoir. We denote by $epsilon$ the characteristic size of the heterogeneity in the medium. A function $alpha$ characterizes the cracking degree of the rock. Our starting point is an adapted microscopic model which is scaled by appropriate powers of $epsilon$. We then study its limit as $epsilon o 0$. Because of the partially fractured character of the medium, the equation expressing the conservation of total mass in the flow is of degenerate parabolic type. The homogenization process for this equation is thus nonstandard. To overcome this difficulty, we adapt two-scale convergence techniques, convexity arguments and classical compactness tools. The homogenized model contains both single porosity and double porosity characteristics. |
topic |
Miscible compressible displacement porous medium partially fractured reservoir double porosity homogenization two-scale limit of a degenerate parabolic equation |
url |
http://ejde.math.txstate.edu/Volumes/2009/01/abstr.html |
work_keys_str_mv |
AT catherinechoquet homogenizedmodelforflowinpartiallyfracturedmedia |
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1724836807832502272 |