Use of stable water isotopes to identify water as a source for palsa ice core formation

Isotopic characteristics of ice cores of peat mounds (palsa) are considered. The distribution of the values of δ18O, δ2H, dexc and ratios δ18O–δ2H within the palza ice lense is associated with freezing in a closed or open system, and this allows finding the source of water for the ice formation. The...

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Bibliographic Details
Main Authors: Yu. N. Chizhova, Yu. K. Vasil’chuk
Format: Article
Language:Russian
Published: Nauka 2020-08-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/818