Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment
In continuous permafrost environments, understanding complex river-talik system dynamics is fundamental for the sustainable use of talik aquifers as a source of drinking water in remote communities. A conceptual model of a river-talik system was previously developed based on field investigations in...
Published in: | Water Resources Research |
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Main Authors: | , , , |
Format: | Other/Unknown Material |
Language: | English |
Published: |
American Geophysical Union
2022
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11794/73041 https://doi.org/10.1029/2021WR031630 |
_version_ | 1826778191099854848 |
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author | Lemieux, Jean-Michel Fortier, Richard Molson, John W. H. Liu, Weibo |
author_facet | Lemieux, Jean-Michel Fortier, Richard Molson, John W. H. Liu, Weibo |
author_sort | Lemieux, Jean-Michel |
collection | Université Laval: CorpusUL |
container_issue | 3 |
container_title | Water Resources Research |
container_volume | 58 |
description | In continuous permafrost environments, understanding complex river-talik system dynamics is fundamental for the sustainable use of talik aquifers as a source of drinking water in remote communities. A conceptual model of a river-talik system was previously developed based on field investigations in the floodplain of the Kuuguluk River at Salluit, Nunavik (Quebec), Canada, including geophysical surveys and monitoring of hydraulic heads and riverbed temperatures. This conceptual model is here used to develop a 3D numerical model for simulating the governing cryo-hydrogeological processes and dynamic system behavior. The numerical simulations, supported by the field data, show that the width and thickness of the river talik is highly correlated to the width of the overlying riverbed. In summer, the river talik is hydraulically connected to the riverbed, and groundwater from the talik aquifer is contributing to river baseflow. In winter, when the river and riverbed freeze, the river talik becomes hydraulically isolated from the riverbed. Under such conditions, the river talik acts as a tube-like conduit system which focusses groundwater flow. Increasing hydraulic heads at constrictions in the talik can be sufficient to fracture the frozen riverbed and ice cover, leading to groundwater overflows and icing formation. This study presents an integrated field and modeling approach for assessing the potential of talik aquifers as reliable sources of drinking water in northern communities. |
format | Other/Unknown Material |
genre | Ice permafrost Salluit Nunavik |
genre_facet | Ice permafrost Salluit Nunavik |
geographic | Nunavik Canada Talik Salluit |
geographic_facet | Nunavik Canada Talik Salluit |
id | ftunivlavalcorp:oai:corpus.ulaval.ca:20.500.11794/73041 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(146.601,146.601,59.667,59.667) ENVELOPE(-75.643,-75.643,62.204,62.204) |
op_collection_id | ftunivlavalcorp |
op_coverage | Canada (Nord) Régions froides |
op_doi | https://doi.org/20.500.11794/7304110.1029/2021WR031630 |
op_relation | https://hdl.handle.net/20.500.11794/73041 doi:10.1029/2021WR031630 |
op_rights | http://purl.org/coar/access_right/c_abf2 |
publishDate | 2022 |
publisher | American Geophysical Union |
record_format | openpolar |
spelling | ftunivlavalcorp:oai:corpus.ulaval.ca:20.500.11794/73041 2025-03-16T15:28:19+00:00 Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment Lemieux, Jean-Michel Fortier, Richard Molson, John W. H. Liu, Weibo Canada (Nord) Régions froides 2022-03-31T20:06:12Z application/pdf https://hdl.handle.net/20.500.11794/73041 https://doi.org/10.1029/2021WR031630 eng eng American Geophysical Union https://hdl.handle.net/20.500.11794/73041 doi:10.1029/2021WR031630 http://purl.org/coar/access_right/c_abf2 Taliks Interaction aquifère-rivière Eau souterraine -- Écoulement -- Méthodes de simulation Chenaux Glace -- Formation Modèles hydrogéologiques Pergélisols Modèles numériques de terrain Glaciologie Eau -- Approvisionnement -- Conditions par temps froid article de recherche COAR1_1::Texte::Périodique::Revue::Contribution à un journal::Article::Article de recherche 2022 ftunivlavalcorp https://doi.org/20.500.11794/7304110.1029/2021WR031630 2025-02-20T15:13:44Z In continuous permafrost environments, understanding complex river-talik system dynamics is fundamental for the sustainable use of talik aquifers as a source of drinking water in remote communities. A conceptual model of a river-talik system was previously developed based on field investigations in the floodplain of the Kuuguluk River at Salluit, Nunavik (Quebec), Canada, including geophysical surveys and monitoring of hydraulic heads and riverbed temperatures. This conceptual model is here used to develop a 3D numerical model for simulating the governing cryo-hydrogeological processes and dynamic system behavior. The numerical simulations, supported by the field data, show that the width and thickness of the river talik is highly correlated to the width of the overlying riverbed. In summer, the river talik is hydraulically connected to the riverbed, and groundwater from the talik aquifer is contributing to river baseflow. In winter, when the river and riverbed freeze, the river talik becomes hydraulically isolated from the riverbed. Under such conditions, the river talik acts as a tube-like conduit system which focusses groundwater flow. Increasing hydraulic heads at constrictions in the talik can be sufficient to fracture the frozen riverbed and ice cover, leading to groundwater overflows and icing formation. This study presents an integrated field and modeling approach for assessing the potential of talik aquifers as reliable sources of drinking water in northern communities. Other/Unknown Material Ice permafrost Salluit Nunavik Université Laval: CorpusUL Nunavik Canada Talik ENVELOPE(146.601,146.601,59.667,59.667) Salluit ENVELOPE(-75.643,-75.643,62.204,62.204) Water Resources Research 58 3 |
spellingShingle | Taliks Interaction aquifère-rivière Eau souterraine -- Écoulement -- Méthodes de simulation Chenaux Glace -- Formation Modèles hydrogéologiques Pergélisols Modèles numériques de terrain Glaciologie Eau -- Approvisionnement -- Conditions par temps froid Lemieux, Jean-Michel Fortier, Richard Molson, John W. H. Liu, Weibo Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title | Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title_full | Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title_fullStr | Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title_full_unstemmed | Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title_short | Three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik System in a continuous permafrost environment |
title_sort | three-dimensional numerical modeling of cryo-hydrogeological processes in a river-talik system in a continuous permafrost environment |
topic | Taliks Interaction aquifère-rivière Eau souterraine -- Écoulement -- Méthodes de simulation Chenaux Glace -- Formation Modèles hydrogéologiques Pergélisols Modèles numériques de terrain Glaciologie Eau -- Approvisionnement -- Conditions par temps froid |
topic_facet | Taliks Interaction aquifère-rivière Eau souterraine -- Écoulement -- Méthodes de simulation Chenaux Glace -- Formation Modèles hydrogéologiques Pergélisols Modèles numériques de terrain Glaciologie Eau -- Approvisionnement -- Conditions par temps froid |
url | https://hdl.handle.net/20.500.11794/73041 https://doi.org/10.1029/2021WR031630 |