Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation

Upscaling of transport properties of heterogeneous porous rocks, such as hydraulic conductivity, is controlled not only by the spatial heterogeneity, but also by the temporal variations of the flow field. Thus effective hydraulic conductivity and permeability of a heterogeneous porous medium is freq...

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Main Authors: Caspari, Eva, Müller, T., Gurevich, Boris
Other Authors: EAGE
Format: Conference Paper
Published: EAGE 2012
Online Access:http://www.earthdoc.org/
http://hdl.handle.net/20.500.11937/33963
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author Caspari, Eva
Müller, T.
Gurevich, Boris
author2 EAGE
author_facet EAGE
Caspari, Eva
Müller, T.
Gurevich, Boris
author_sort Caspari, Eva
building Curtin Institutional Repository
collection Online Access
description Upscaling of transport properties of heterogeneous porous rocks, such as hydraulic conductivity, is controlled not only by the spatial heterogeneity, but also by the temporal variations of the flow field. Thus effective hydraulic conductivity and permeability of a heterogeneous porous medium is frequency dependent. Existing upscaling methods for this property are often limited to small spatial variations of permeability, which is a significant limitation. In this study we apply a strong contrast expansion method, originally suggested in the context of the dynamic dielectric constant, to the problem of upscaling hydraulic conductivity in a 1D random medium. A closed-form expression for the effective hydraulic conductivity, which depends on the second order statistics, is derived. Unlike the small contrast approximations, in the low- and high-frequency limits this new expression yields harmonic and arithmetic averages of permeability, respectively, which are known to be exact low- and high-frequency limits in 1D.
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institution Curtin University Malaysia
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spelling curtin-20.500.11937-339632017-01-30T13:40:27Z Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation Caspari, Eva Müller, T. Gurevich, Boris EAGE Upscaling of transport properties of heterogeneous porous rocks, such as hydraulic conductivity, is controlled not only by the spatial heterogeneity, but also by the temporal variations of the flow field. Thus effective hydraulic conductivity and permeability of a heterogeneous porous medium is frequency dependent. Existing upscaling methods for this property are often limited to small spatial variations of permeability, which is a significant limitation. In this study we apply a strong contrast expansion method, originally suggested in the context of the dynamic dielectric constant, to the problem of upscaling hydraulic conductivity in a 1D random medium. A closed-form expression for the effective hydraulic conductivity, which depends on the second order statistics, is derived. Unlike the small contrast approximations, in the low- and high-frequency limits this new expression yields harmonic and arithmetic averages of permeability, respectively, which are known to be exact low- and high-frequency limits in 1D. 2012 Conference Paper http://hdl.handle.net/20.500.11937/33963 http://www.earthdoc.org/ http://www.earthdoc.org/publication/publicationdetails/?publication=59181 EAGE fulltext
spellingShingle Caspari, Eva
Müller, T.
Gurevich, Boris
Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title_full Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title_fullStr Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title_full_unstemmed Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title_short Frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
title_sort frequency-dependent effective hydraulic conductivity in randomly layered porous medium - strong contrast approximation
url http://www.earthdoc.org/
http://www.earthdoc.org/
http://hdl.handle.net/20.500.11937/33963