Can Deep Groundwater Influx be Detected from the Geochemistry of Thermokarst Lakes in Arctic Alaska?

Abstract 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 la...

Full description

Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Hinkel, Kenneth M., Arp, Christopher D., Townsend‐Small, Amy, Frey, Karen E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.1895
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1895
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1895