Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations
In geochemically reacting environments, the mineral dissolution and precipitation alters the structural and transport properties of the media of interest. The chemical and structural heterogeneities of the porous media affect the temporal evolution of the permeability with respect to porosity. Such...
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2018-01-01
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Series: | Geofluids |
Online Access: | http://dx.doi.org/10.1155/2018/9260603 |
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doaj-cceaefd9f2f64cd49794e27ca6409e912020-11-25T02:26:49ZengHindawi-WileyGeofluids1468-81151468-81232018-01-01201810.1155/2018/92606039260603Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale SimulationsNikolaos I. Prasianakis0Michael Gatschet1Aida Abbasi2Sergey V. Churakov3Laboratory for Waste Management LES, Nuclear Energy and Safety Department, Paul Scherrer Institute, 5232 Villigen, SwitzerlandLaboratory for Waste Management LES, Nuclear Energy and Safety Department, Paul Scherrer Institute, 5232 Villigen, SwitzerlandLaboratory for Waste Management LES, Nuclear Energy and Safety Department, Paul Scherrer Institute, 5232 Villigen, SwitzerlandLaboratory for Waste Management LES, Nuclear Energy and Safety Department, Paul Scherrer Institute, 5232 Villigen, SwitzerlandIn geochemically reacting environments, the mineral dissolution and precipitation alters the structural and transport properties of the media of interest. The chemical and structural heterogeneities of the porous media affect the temporal evolution of the permeability with respect to porosity. Such correlations follow a nonlinear trend, which is difficult to estimate a priori and without knowledge of the microstructure itself, especially under the presence of strong chemical gradients. Macroscopic field-scale codes require such an input, and in the absence of exact descriptions, simplified correlations are used. After highlighting the diversity of microstructural evolution paths, due to dissolution, we discuss possible upscaling strategies.http://dx.doi.org/10.1155/2018/9260603 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Nikolaos I. Prasianakis Michael Gatschet Aida Abbasi Sergey V. Churakov |
spellingShingle |
Nikolaos I. Prasianakis Michael Gatschet Aida Abbasi Sergey V. Churakov Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations Geofluids |
author_facet |
Nikolaos I. Prasianakis Michael Gatschet Aida Abbasi Sergey V. Churakov |
author_sort |
Nikolaos I. Prasianakis |
title |
Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations |
title_short |
Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations |
title_full |
Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations |
title_fullStr |
Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations |
title_full_unstemmed |
Upscaling Strategies of Porosity-Permeability Correlations in Reacting Environments from Pore-Scale Simulations |
title_sort |
upscaling strategies of porosity-permeability correlations in reacting environments from pore-scale simulations |
publisher |
Hindawi-Wiley |
series |
Geofluids |
issn |
1468-8115 1468-8123 |
publishDate |
2018-01-01 |
description |
In geochemically reacting environments, the mineral dissolution and precipitation alters the structural and transport properties of the media of interest. The chemical and structural heterogeneities of the porous media affect the temporal evolution of the permeability with respect to porosity. Such correlations follow a nonlinear trend, which is difficult to estimate a priori and without knowledge of the microstructure itself, especially under the presence of strong chemical gradients. Macroscopic field-scale codes require such an input, and in the absence of exact descriptions, simplified correlations are used. After highlighting the diversity of microstructural evolution paths, due to dissolution, we discuss possible upscaling strategies. |
url |
http://dx.doi.org/10.1155/2018/9260603 |
work_keys_str_mv |
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1724845538003648512 |