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: Kenneth M. Hinkel, Christopher D. Arp, Amy Townsend‐Small, Karen E. Frey
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/ppp.1895