Coupled Transport in Natural Porous Media (2. rev. Ed.)
As the interactions between transport processes are important for a number of interesting systems, a set of partial differential equations and appropriate parameter functions for the study of coupled water, heat, gas and solute transport was formulated and a state of the art computer model for the n...
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ftunivheidelb:oai:archiv.ub.uni-heidelberg.de:3220 2023-11-05T03:44:36+01:00 Coupled Transport in Natural Porous Media (2. rev. Ed.) Ippisch, Olaf 2001 application/pdf https://archiv.ub.uni-heidelberg.de/volltextserver/3220/ https://archiv.ub.uni-heidelberg.de/volltextserver/3220/1/coupled_transport_in_natural_porous_media.pdf https://archiv.ub.uni-heidelberg.de/volltextserver/3220/2/erratum_et_addendum.pdf https://doi.org/10.11588/heidok.00003220 https://nbn-resolving.org/urn:nbn:de:bsz:16-heidok-32208 eng eng https://archiv.ub.uni-heidelberg.de/volltextserver/3220/1/coupled_transport_in_natural_porous_media.pdf https://archiv.ub.uni-heidelberg.de/volltextserver/3220/2/erratum_et_addendum.pdf doi:10.11588/heidok.00003220 urn:nbn:de:bsz:16-heidok-32208 Ippisch, Olaf (2001) Coupled Transport in Natural Porous Media (2. rev. Ed.). . info:eu-repo/semantics/openAccess http://archiv.ub.uni-heidelberg.de/volltextserver/help/license_urhg.html 550 550 Earth sciences Book info:eu-repo/semantics/book NonPeerReviewed 2001 ftunivheidelb https://doi.org/10.11588/heidok.00003220 2023-10-10T12:04:38Z As the interactions between transport processes are important for a number of interesting systems, a set of partial differential equations and appropriate parameter functions for the study of coupled water, heat, gas and solute transport was formulated and a state of the art computer model for the numerical solution of the equation system was created. A new phase pressure/partial pressure formulation for the coupled transport of liquid and gas phase was developed. The model was used to simulate the water and energy dynamics of a permafrost soil. A good qualitative agreement was achieved. Differences between modeled and measured data could be explained with heterogeneity in combination with the model's sensitivity to a change in hydraulic parameters. Water vapor and solute transport had no effect on the simulation result but transport of liquid water proved to be an important heat transfer process near 0 °C. The impact of the chosen parameterization and model on the simulation of a multistep outflow experiment was analyzed. Differences between a model based on Richards' equation and a twophase model only occurred when the Brooks-Corey parameterization was used. The results of the twophase model showed a retarded drainage and a hysteresis during imbibation which is in good agreement with experimental results. Book permafrost Heidelberg University: HeiDok |
institution |
Open Polar |
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Heidelberg University: HeiDok |
op_collection_id |
ftunivheidelb |
language |
English |
topic |
550 550 Earth sciences |
spellingShingle |
550 550 Earth sciences Ippisch, Olaf Coupled Transport in Natural Porous Media (2. rev. Ed.) |
topic_facet |
550 550 Earth sciences |
description |
As the interactions between transport processes are important for a number of interesting systems, a set of partial differential equations and appropriate parameter functions for the study of coupled water, heat, gas and solute transport was formulated and a state of the art computer model for the numerical solution of the equation system was created. A new phase pressure/partial pressure formulation for the coupled transport of liquid and gas phase was developed. The model was used to simulate the water and energy dynamics of a permafrost soil. A good qualitative agreement was achieved. Differences between modeled and measured data could be explained with heterogeneity in combination with the model's sensitivity to a change in hydraulic parameters. Water vapor and solute transport had no effect on the simulation result but transport of liquid water proved to be an important heat transfer process near 0 °C. The impact of the chosen parameterization and model on the simulation of a multistep outflow experiment was analyzed. Differences between a model based on Richards' equation and a twophase model only occurred when the Brooks-Corey parameterization was used. The results of the twophase model showed a retarded drainage and a hysteresis during imbibation which is in good agreement with experimental results. |
format |
Book |
author |
Ippisch, Olaf |
author_facet |
Ippisch, Olaf |
author_sort |
Ippisch, Olaf |
title |
Coupled Transport in Natural Porous Media (2. rev. Ed.) |
title_short |
Coupled Transport in Natural Porous Media (2. rev. Ed.) |
title_full |
Coupled Transport in Natural Porous Media (2. rev. Ed.) |
title_fullStr |
Coupled Transport in Natural Porous Media (2. rev. Ed.) |
title_full_unstemmed |
Coupled Transport in Natural Porous Media (2. rev. Ed.) |
title_sort |
coupled transport in natural porous media (2. rev. ed.) |
publishDate |
2001 |
url |
https://archiv.ub.uni-heidelberg.de/volltextserver/3220/ https://archiv.ub.uni-heidelberg.de/volltextserver/3220/1/coupled_transport_in_natural_porous_media.pdf https://archiv.ub.uni-heidelberg.de/volltextserver/3220/2/erratum_et_addendum.pdf https://doi.org/10.11588/heidok.00003220 https://nbn-resolving.org/urn:nbn:de:bsz:16-heidok-32208 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
https://archiv.ub.uni-heidelberg.de/volltextserver/3220/1/coupled_transport_in_natural_porous_media.pdf https://archiv.ub.uni-heidelberg.de/volltextserver/3220/2/erratum_et_addendum.pdf doi:10.11588/heidok.00003220 urn:nbn:de:bsz:16-heidok-32208 Ippisch, Olaf (2001) Coupled Transport in Natural Porous Media (2. rev. Ed.). . |
op_rights |
info:eu-repo/semantics/openAccess http://archiv.ub.uni-heidelberg.de/volltextserver/help/license_urhg.html |
op_doi |
https://doi.org/10.11588/heidok.00003220 |
_version_ |
1781704919888166912 |