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...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Hinkel, Kenneth M, Arp, Christopher D., Townsend-Small, Amy, Frey, Karen E.
Format: Text
Language:unknown
Published: Digital Commons @ Michigan Tech 2017
Subjects:
Online Access:https://digitalcommons.mtu.edu/michigantech-p/3854
https://doi.org/10.1002/ppp.1895