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...

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Published in:Water Resources Research
Main Authors: Lemieux, Jean-Michel, Fortier, Richard, Molson, John W. H., Liu, Weibo
Format: Other/Unknown Material
Language:English
Published: American Geophysical Union 2022
Subjects:
Online Access:https://hdl.handle.net/20.500.11794/73041
https://doi.org/10.1029/2021WR031630
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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
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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
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publisher American Geophysical Union
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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