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author Jamin, P.
Cochand, M.
Dagenais, S.
Lemieux, J.-M.
Fortier, R.
Molson, J.
Brouyère, S.
author2 Fonds De La Recherche Scientifique - FNRS
Natural Sciences and Engineering Research Council of Canada
Koning Boudewijnstichting
Université de Liège
author_facet Jamin, P.
Cochand, M.
Dagenais, S.
Lemieux, J.-M.
Fortier, R.
Molson, J.
Brouyère, S.
author_sort Jamin, P.
collection Springer Nature
container_issue 3
container_start_page 869
container_title Hydrogeology Journal
container_volume 28
format Article in Journal/Newspaper
genre permafrost
Umiujaq
Nunavik
genre_facet permafrost
Umiujaq
Nunavik
geographic Canada
Nunavik
Umiujaq
geographic_facet Canada
Nunavik
Umiujaq
id crspringernat:10.1007/s10040-020-02108-y
institution Open Polar
language English
long_lat ENVELOPE(-76.549,-76.549,56.553,56.553)
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op_container_end_page 885
op_doi https://doi.org/10.1007/s10040-020-02108-y
op_rights http://www.springer.com/tdm
http://www.springer.com/tdm
op_source Hydrogeology Journal
volume 28, issue 3, page 869-885
ISSN 1431-2174 1435-0157
publishDate 2020
publisher Springer Science and Business Media LLC
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spelling crspringernat:10.1007/s10040-020-02108-y 2025-01-17T00:15:02+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, P. Cochand, M. Dagenais, S. Lemieux, J.-M. Fortier, R. Molson, J. Brouyère, S. Fonds De La Recherche Scientifique - FNRS Natural Sciences and Engineering Research Council of Canada Koning Boudewijnstichting Université de Liège 2020 http://dx.doi.org/10.1007/s10040-020-02108-y http://link.springer.com/content/pdf/10.1007/s10040-020-02108-y.pdf http://link.springer.com/article/10.1007/s10040-020-02108-y/fulltext.html en eng Springer Science and Business Media LLC http://www.springer.com/tdm http://www.springer.com/tdm Hydrogeology Journal volume 28, issue 3, page 869-885 ISSN 1431-2174 1435-0157 Earth and Planetary Sciences (miscellaneous) Water Science and Technology journal-article 2020 crspringernat https://doi.org/10.1007/s10040-020-02108-y 2022-01-04T14:08:50Z Article in Journal/Newspaper permafrost Umiujaq Nunavik Springer Nature Canada Nunavik Umiujaq ENVELOPE(-76.549,-76.549,56.553,56.553) Hydrogeology Journal 28 3 869 885
spellingShingle Earth and Planetary Sciences (miscellaneous)
Water Science and Technology
Jamin, P.
Cochand, M.
Dagenais, S.
Lemieux, J.-M.
Fortier, R.
Molson, J.
Brouyère, S.
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 Earth and Planetary Sciences (miscellaneous)
Water Science and Technology
topic_facet Earth and Planetary Sciences (miscellaneous)
Water Science and Technology
url http://dx.doi.org/10.1007/s10040-020-02108-y
http://link.springer.com/content/pdf/10.1007/s10040-020-02108-y.pdf
http://link.springer.com/article/10.1007/s10040-020-02108-y/fulltext.html