On the validity of effective formulations for transport through heterogeneous porous media

Geological heterogeneity enhances spreading of solutes and causes transport to be anomalous (i.e., non-Fickian), with much less mixing than suggested by dispersion. This implies that modeling transport requires adopting either stochastic approaches that model heterogeneity explicitly or effective transport formulations that acknowledge the effects of heterogeneity. A number of such formulations have been developed and tested as upscaled representations of enhanced spreading. However, their ability to represent mixing has not been formally tested, which is required for proper reproduction of chemical reactions and which motivates our work. We propose that, for an effective transport formulation to be considered a valid representation of transport through heterogeneous porous media (HPM), it should honor mean advection, mixing and spreading. It should also be flexible enough to be applicable to real problems. We test the capacity of the multi-rate mass transfer (MRMT) model to reproduce mixing observed in HPM, as represented by the classical multi-Gaussian log-permeability field with a Gaussian correlation pattern. Non-dispersive mixing comes from heterogeneity structures in the concentration fields that are not captured by macrodispersion. These fine structures limit mixing initially, but eventually enhance it. Numerical results show that, relative to HPM, MRMT models display a much stronger memory of initial conditions on mixing than on dispersion because of the sensitivity of the mixing state to the actual values of concentration. Because MRMT does not restitute the local concentration structures, it induces smaller non-dispersive mixing than HPM. However long-lived trapping in the immobile zones may sustain the deviation from dispersive mixing over much longer times. While spreading can be well captured by MRMT models, in general non-dispersive mixing cannot. © Author(s) 2016.

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Bibliographic Details
Main Authors: De Dreuzy, Jean Raynald, Carrera, Jesús
Other Authors: European Research Council
Format: artículo biblioteca
Language:English
Published: Copernicus Publications 2016-04-05
Subjects:Porous materials, Solute transport, Dispersion coefficient, Mass transfer,
Online Access:http://hdl.handle.net/10261/175385
http://dx.doi.org/10.13039/501100000781
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spelling dig-idaea-es-10261-1753852021-08-18T10:46:45Z On the validity of effective formulations for transport through heterogeneous porous media De Dreuzy, Jean Raynald Carrera, Jesús European Research Council Porous materials Solute transport Dispersion coefficient Mass transfer Geological heterogeneity enhances spreading of solutes and causes transport to be anomalous (i.e., non-Fickian), with much less mixing than suggested by dispersion. This implies that modeling transport requires adopting either stochastic approaches that model heterogeneity explicitly or effective transport formulations that acknowledge the effects of heterogeneity. A number of such formulations have been developed and tested as upscaled representations of enhanced spreading. However, their ability to represent mixing has not been formally tested, which is required for proper reproduction of chemical reactions and which motivates our work. We propose that, for an effective transport formulation to be considered a valid representation of transport through heterogeneous porous media (HPM), it should honor mean advection, mixing and spreading. It should also be flexible enough to be applicable to real problems. We test the capacity of the multi-rate mass transfer (MRMT) model to reproduce mixing observed in HPM, as represented by the classical multi-Gaussian log-permeability field with a Gaussian correlation pattern. Non-dispersive mixing comes from heterogeneity structures in the concentration fields that are not captured by macrodispersion. These fine structures limit mixing initially, but eventually enhance it. Numerical results show that, relative to HPM, MRMT models display a much stronger memory of initial conditions on mixing than on dispersion because of the sensitivity of the mixing state to the actual values of concentration. Because MRMT does not restitute the local concentration structures, it induces smaller non-dispersive mixing than HPM. However long-lived trapping in the immobile zones may sustain the deviation from dispersive mixing over much longer times. While spreading can be well captured by MRMT models, in general non-dispersive mixing cannot. © Author(s) 2016. The European Union is acknowledged for its funding through the Marie-Curie Fellowship PIEF-GA-2009-251710 and through the project FP7-ENERGY-2012-1-2STAGE TRUST (High-resolution monitoring, real time visualization and reliable modeling of highly controlled, intermediate and upscalable size pilot injection tests of underground storage of CO2). The ANR is acknowledged for its funding through its Project H2MNO4 under the No. ANR-12-MONU-0012-01. Peer reviewed 2019-02-06T11:06:11Z 2019-02-06T11:06:11Z 2016-04-05 artículo http://purl.org/coar/resource_type/c_6501 Hydrology and Earth System Sciences 20 (4): 1319-1330 (2016) http://hdl.handle.net/10261/175385 10.5194/hess-20-1319-2016 http://dx.doi.org/10.13039/501100000781 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/FP7/309067 Publisher's version https://doi.org/10.5194/hess-20-1319-2016 Sí open Copernicus Publications
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Porous materials
Solute transport
Dispersion coefficient
Mass transfer
Porous materials
Solute transport
Dispersion coefficient
Mass transfer
spellingShingle Porous materials
Solute transport
Dispersion coefficient
Mass transfer
Porous materials
Solute transport
Dispersion coefficient
Mass transfer
De Dreuzy, Jean Raynald
Carrera, Jesús
On the validity of effective formulations for transport through heterogeneous porous media
description Geological heterogeneity enhances spreading of solutes and causes transport to be anomalous (i.e., non-Fickian), with much less mixing than suggested by dispersion. This implies that modeling transport requires adopting either stochastic approaches that model heterogeneity explicitly or effective transport formulations that acknowledge the effects of heterogeneity. A number of such formulations have been developed and tested as upscaled representations of enhanced spreading. However, their ability to represent mixing has not been formally tested, which is required for proper reproduction of chemical reactions and which motivates our work. We propose that, for an effective transport formulation to be considered a valid representation of transport through heterogeneous porous media (HPM), it should honor mean advection, mixing and spreading. It should also be flexible enough to be applicable to real problems. We test the capacity of the multi-rate mass transfer (MRMT) model to reproduce mixing observed in HPM, as represented by the classical multi-Gaussian log-permeability field with a Gaussian correlation pattern. Non-dispersive mixing comes from heterogeneity structures in the concentration fields that are not captured by macrodispersion. These fine structures limit mixing initially, but eventually enhance it. Numerical results show that, relative to HPM, MRMT models display a much stronger memory of initial conditions on mixing than on dispersion because of the sensitivity of the mixing state to the actual values of concentration. Because MRMT does not restitute the local concentration structures, it induces smaller non-dispersive mixing than HPM. However long-lived trapping in the immobile zones may sustain the deviation from dispersive mixing over much longer times. While spreading can be well captured by MRMT models, in general non-dispersive mixing cannot. © Author(s) 2016.
author2 European Research Council
author_facet European Research Council
De Dreuzy, Jean Raynald
Carrera, Jesús
format artículo
topic_facet Porous materials
Solute transport
Dispersion coefficient
Mass transfer
author De Dreuzy, Jean Raynald
Carrera, Jesús
author_sort De Dreuzy, Jean Raynald
title On the validity of effective formulations for transport through heterogeneous porous media
title_short On the validity of effective formulations for transport through heterogeneous porous media
title_full On the validity of effective formulations for transport through heterogeneous porous media
title_fullStr On the validity of effective formulations for transport through heterogeneous porous media
title_full_unstemmed On the validity of effective formulations for transport through heterogeneous porous media
title_sort on the validity of effective formulations for transport through heterogeneous porous media
publisher Copernicus Publications
publishDate 2016-04-05
url http://hdl.handle.net/10261/175385
http://dx.doi.org/10.13039/501100000781
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