Can Deep Groundwater Influx be Detected from the Geochemistry of Thermokarst Lakes in Arctic Alaska?
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub-lake taliks that extend through permafrost provide a potential conduit for subpermafrost groundwater to reach the surface, increasing dissolved ion concentrations in lake water. Twenty-eight lakes on th...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , |
Format: | Text |
Language: | unknown |
Published: |
Digital Commons @ Michigan Tech
2017
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Subjects: | |
Online Access: | https://digitalcommons.mtu.edu/michigantech-p/3854 https://doi.org/10.1002/ppp.1895 |