Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada)
Permafrost thaw is a complex process resulting from interactions between the atmosphere, soil, water and vegetation. Although advective heat transport by groundwater at depth likely plays a significant role in permafrost dynamics at many sites, there is lack of direct measurements of groundwater flo...
Published in: | Hydrogeology Journal |
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Main Authors: | , , , , , , |
Format: | Other/Unknown Material |
Language: | English |
Published: |
Springer
2020
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11794/38753 https://doi.org/10.1007/s10040-020-02108-y |
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author | Jamin, Pierre Cochand, Marion Lemieux, Jean-Michel Dagenais, Sophie Fortier, Richard Brouyère, Serge Molson, John W. H. |
author_facet | Jamin, Pierre Cochand, Marion Lemieux, Jean-Michel Dagenais, Sophie Fortier, Richard Brouyère, Serge Molson, John W. H. |
author_sort | Jamin, Pierre |
collection | Université Laval: CorpusUL |
container_issue | 3 |
container_start_page | 869 |
container_title | Hydrogeology Journal |
container_volume | 28 |
description | Permafrost thaw is a complex process resulting from interactions between the atmosphere, soil, water and vegetation. Although advective heat transport by groundwater at depth likely plays a significant role in permafrost dynamics at many sites, there is lack of direct measurements of groundwater flow patterns and fluxes in such cold-region environments. Here, the finite volume point dilution method (FVPDM) is used to measure in-situ groundwater fluxes in two sandy aquifers in the discontinuous permafrost zone, within a small watershed near Umiujaq, Nunavik (Quebec), Canada. The FVPDM theory is first reviewed, then results from four FVPDM tests are presented: one test in a shallow supra-permafrost aquifer, and three in a deeper subpermafrost aquifer. Apparent Darcy fluxes derived from the FVPDM tests varied from 0.5 × 10−5 to 1.0 × 10−5 m/s, implying that advective heat transport from groundwater flow could be contributing to rapid permafrost thaw at this site. In providing estimates of the Darcy fluxes at the local scale of the well screens, the approach offers more accurate and direct measurements over indirect estimates using Darcy’s law. The tests show that this method can be successfully used in remote areas and with limited resources. Recommendations for optimizing the test protocol are proposed. |
format | Other/Unknown Material |
genre | permafrost Umiujaq Nunavik |
genre_facet | permafrost Umiujaq Nunavik |
geographic | Canada Nunavik Umiujaq |
geographic_facet | Canada Nunavik Umiujaq |
id | ftunivlavalcorp:oai:corpus.ulaval.ca:20.500.11794/38753 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-76.549,-76.549,56.553,56.553) |
op_collection_id | ftunivlavalcorp |
op_container_end_page | 885 |
op_coverage | Québec (Province) -- Umiujaq |
op_doi | https://doi.org/20.500.11794/3875310.1007/s10040-020-02108-y |
op_relation | https://hdl.handle.net/20.500.11794/38753 |
op_rights | http://purl.org/coar/access_right/c_16ec |
publishDate | 2020 |
publisher | Springer |
record_format | openpolar |
spelling | ftunivlavalcorp:oai:corpus.ulaval.ca:20.500.11794/38753 2025-05-18T14:06:12+00:00 Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) Jamin, Pierre Cochand, Marion Lemieux, Jean-Michel Dagenais, Sophie Fortier, Richard Brouyère, Serge Molson, John W. H. Québec (Province) -- Umiujaq 2020-04-15T15:08:49Z application/pdf https://hdl.handle.net/20.500.11794/38753 https://doi.org/10.1007/s10040-020-02108-y eng eng Springer https://hdl.handle.net/20.500.11794/38753 http://purl.org/coar/access_right/c_16ec Finite volume point dilution method Tracer test Groundwater flow Permafrost Canada Méthodes de volumes finis Eau souterraine -- Écoulement Pergélisols Aquifères article de recherche COAR1_1::Texte::Périodique::Revue::Contribution à un journal::Article::Article de recherche 2020 ftunivlavalcorp https://doi.org/20.500.11794/3875310.1007/s10040-020-02108-y 2025-04-28T00:28:27Z Permafrost thaw is a complex process resulting from interactions between the atmosphere, soil, water and vegetation. Although advective heat transport by groundwater at depth likely plays a significant role in permafrost dynamics at many sites, there is lack of direct measurements of groundwater flow patterns and fluxes in such cold-region environments. Here, the finite volume point dilution method (FVPDM) is used to measure in-situ groundwater fluxes in two sandy aquifers in the discontinuous permafrost zone, within a small watershed near Umiujaq, Nunavik (Quebec), Canada. The FVPDM theory is first reviewed, then results from four FVPDM tests are presented: one test in a shallow supra-permafrost aquifer, and three in a deeper subpermafrost aquifer. Apparent Darcy fluxes derived from the FVPDM tests varied from 0.5 × 10−5 to 1.0 × 10−5 m/s, implying that advective heat transport from groundwater flow could be contributing to rapid permafrost thaw at this site. In providing estimates of the Darcy fluxes at the local scale of the well screens, the approach offers more accurate and direct measurements over indirect estimates using Darcy’s law. The tests show that this method can be successfully used in remote areas and with limited resources. Recommendations for optimizing the test protocol are proposed. Other/Unknown Material permafrost Umiujaq Nunavik Université Laval: CorpusUL Canada Nunavik Umiujaq ENVELOPE(-76.549,-76.549,56.553,56.553) Hydrogeology Journal 28 3 869 885 |
spellingShingle | Finite volume point dilution method Tracer test Groundwater flow Permafrost Canada Méthodes de volumes finis Eau souterraine -- Écoulement Pergélisols Aquifères Jamin, Pierre Cochand, Marion Lemieux, Jean-Michel Dagenais, Sophie Fortier, Richard Brouyère, Serge Molson, John W. H. Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title | Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title_full | Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title_fullStr | Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title_full_unstemmed | Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title_short | Direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near Umiujaq (Nunavik, Canada) |
title_sort | direct measurement of groundwater flux in aquifers within the discontinuous permafrost zone: an application of the finite volume point dilution method near umiujaq (nunavik, canada) |
topic | Finite volume point dilution method Tracer test Groundwater flow Permafrost Canada Méthodes de volumes finis Eau souterraine -- Écoulement Pergélisols Aquifères |
topic_facet | Finite volume point dilution method Tracer test Groundwater flow Permafrost Canada Méthodes de volumes finis Eau souterraine -- Écoulement Pergélisols Aquifères |
url | https://hdl.handle.net/20.500.11794/38753 https://doi.org/10.1007/s10040-020-02108-y |