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 |