A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater
International audience The past few decades have seen a rapid development and progress in research on past and current hydrologic impacts of permafrost evolution. In permafrost area, groundwater is subdivided into two zones: supra-permafrost and sub-permafrost which are separated by permafrost. Know...
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Language: | English |
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HAL CCSD
2013
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Online Access: | https://hal.science/hal-01396681 https://hal.science/hal-01396681/document https://hal.science/hal-01396681/file/AGU2013_Paris_v2.pdf |
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ftsorbonneuniv:oai:HAL:hal-01396681v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
HAL Sorbonne Université |
op_collection_id |
ftsorbonneuniv |
language |
English |
topic |
Modeling Climate impacts Permafrost Periglacial processes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology |
spellingShingle |
Modeling Climate impacts Permafrost Periglacial processes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology Rivière, Agnès Jost, Anne Goncalvès, Julio A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
topic_facet |
Modeling Climate impacts Permafrost Periglacial processes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology |
description |
International audience The past few decades have seen a rapid development and progress in research on past and current hydrologic impacts of permafrost evolution. In permafrost area, groundwater is subdivided into two zones: supra-permafrost and sub-permafrost which are separated by permafrost. Knowledge of the sub-permafrost aquifers is often lacking due to the difficulty to access those systems. The few available data show that this aquifers are generally artesian below the continuous permafrost. In the literature, there are two plausible explanations for the relatively high pore pressures in the sub-permafrost aquifer; the recharge related to the ice sheet melting and the expulsion of water related to the ice expansion. In this study, we investigated areas where ice sheets have never developed like in the Paris basin region. The ice expansion induces also soil surface uplift. Our study focuses on modifications of pore water pressure in the sub-permafrost aquifer and the soil surface motion during the permafrost development (freezing front deepening). To fill in the gaps to the field data availability, we developed an experimental approach. Experimental design was undertaken at the Laboratory M2C (Université de Caen-Basse Normandie, CNRS, France). The device consisted in a 2 m2 box insulated at all sides except on the top where a surface temperature was prescribed. The box is filled with silty sand of which hydraulics and thermal parameters are known. Soil temperatures, pore water pressure and soil motion are continuously recorded at different elevations in the sand-box. We developed a two-dimensional transient fully coupled heat and water transport model to simulate thawing and freezing processes taking into account the phase change (Latent heat effects). The balance equations are solved using of a finite difference numerical scheme. Experimental results are used to verify the implementation of the hydro-mechanical processes in our numerical simulations. Experimental and numerical approaches allowed us to ... |
author2 |
University of Calgary Centre de Géosciences (GEOSCIENCES) Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE) Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Milieux Environnementaux, Transferts et Interactions dans les hydrosystèmes et les Sols (METIS) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Conference Object |
author |
Rivière, Agnès Jost, Anne Goncalvès, Julio |
author_facet |
Rivière, Agnès Jost, Anne Goncalvès, Julio |
author_sort |
Rivière, Agnès |
title |
A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
title_short |
A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
title_full |
A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
title_fullStr |
A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
title_full_unstemmed |
A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
title_sort |
combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-01396681 https://hal.science/hal-01396681/document https://hal.science/hal-01396681/file/AGU2013_Paris_v2.pdf |
op_coverage |
San Francisco, United States |
genre |
Ice Ice Sheet permafrost |
genre_facet |
Ice Ice Sheet permafrost |
op_source |
CryosphereHydrological Response to Climate Change in Permafrost Regions II Posters AGU Fall Meeting 2013 https://hal.science/hal-01396681 AGU Fall Meeting 2013, Dec 2013, San Francisco, United States. pp.abstract C53A-0551 http://abstractsearch.agu.org/meetings/2013/FM/C53A-0551.html |
op_relation |
hal-01396681 https://hal.science/hal-01396681 https://hal.science/hal-01396681/document https://hal.science/hal-01396681/file/AGU2013_Paris_v2.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1799481409577943040 |
spelling |
ftsorbonneuniv:oai:HAL:hal-01396681v1 2024-05-19T07:41:48+00:00 A combined experimental and numerical study of pore water pressure variations in sub -permafrost groundwater Rivière, Agnès Jost, Anne Goncalvès, Julio University of Calgary Centre de Géosciences (GEOSCIENCES) Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Structure et fonctionnement des systèmes hydriques continentaux (SISYPHE) Université Pierre et Marie Curie - Paris 6 (UPMC)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Mines Paris - PSL (École nationale supérieure des mines de Paris) Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Milieux Environnementaux, Transferts et Interactions dans les hydrosystèmes et les Sols (METIS) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) San Francisco, United States 2013-12-09 https://hal.science/hal-01396681 https://hal.science/hal-01396681/document https://hal.science/hal-01396681/file/AGU2013_Paris_v2.pdf en eng HAL CCSD hal-01396681 https://hal.science/hal-01396681 https://hal.science/hal-01396681/document https://hal.science/hal-01396681/file/AGU2013_Paris_v2.pdf info:eu-repo/semantics/OpenAccess CryosphereHydrological Response to Climate Change in Permafrost Regions II Posters AGU Fall Meeting 2013 https://hal.science/hal-01396681 AGU Fall Meeting 2013, Dec 2013, San Francisco, United States. pp.abstract C53A-0551 http://abstractsearch.agu.org/meetings/2013/FM/C53A-0551.html Modeling Climate impacts Permafrost Periglacial processes [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDU.STU]Sciences of the Universe [physics]/Earth Sciences [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology info:eu-repo/semantics/conferenceObject Conference papers 2013 ftsorbonneuniv 2024-04-25T04:13:44Z International audience The past few decades have seen a rapid development and progress in research on past and current hydrologic impacts of permafrost evolution. In permafrost area, groundwater is subdivided into two zones: supra-permafrost and sub-permafrost which are separated by permafrost. Knowledge of the sub-permafrost aquifers is often lacking due to the difficulty to access those systems. The few available data show that this aquifers are generally artesian below the continuous permafrost. In the literature, there are two plausible explanations for the relatively high pore pressures in the sub-permafrost aquifer; the recharge related to the ice sheet melting and the expulsion of water related to the ice expansion. In this study, we investigated areas where ice sheets have never developed like in the Paris basin region. The ice expansion induces also soil surface uplift. Our study focuses on modifications of pore water pressure in the sub-permafrost aquifer and the soil surface motion during the permafrost development (freezing front deepening). To fill in the gaps to the field data availability, we developed an experimental approach. Experimental design was undertaken at the Laboratory M2C (Université de Caen-Basse Normandie, CNRS, France). The device consisted in a 2 m2 box insulated at all sides except on the top where a surface temperature was prescribed. The box is filled with silty sand of which hydraulics and thermal parameters are known. Soil temperatures, pore water pressure and soil motion are continuously recorded at different elevations in the sand-box. We developed a two-dimensional transient fully coupled heat and water transport model to simulate thawing and freezing processes taking into account the phase change (Latent heat effects). The balance equations are solved using of a finite difference numerical scheme. Experimental results are used to verify the implementation of the hydro-mechanical processes in our numerical simulations. Experimental and numerical approaches allowed us to ... Conference Object Ice Ice Sheet permafrost HAL Sorbonne Université |