Major ions and dissolved salts in syngenetic ice wedges from Ledovy Obryv and Ust'-Algan outcrops in Mayn River Valley

Major ions and dissolved salts in syngenetic ice wedges in the 25–30 m thick Late Pleistocene Ledovy Obryv yedoma and the 60-m thick Ust'-Algan Obryv yedoma. Analysis of major ion chemistry of ice - titration methods (titrimetric methods) are based on determining the quantity of a reagent of kn...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Vasil'chuk, Alla Constantinovna
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2020
Subjects:
deuterium
heavy oxygen
Holocene
Ice wedges
Late Pleistocene
Mayn River
permafrost
pollen and spores
radiocarbon
Southern Chukchi Peninsula
Stable isotopes
Event label
Latitude of event
Longitude of event
ELEVATION
Sample ID
Sample type
Total dissolved solids
Bicarbonate ion
Chloride
Sulfate
Calcium
Magnesium
Sodium and potassium ions
pH
Chloride/sulfate ratio
Sample comment
Titration
Algan
Mayn
Chukchi
Chukchi Peninsula
Ice
wedge*
Online Access:https://dx.doi.org/10.1594/pangaea.915018
https://doi.pangaea.de/10.1594/PANGAEA.915018
Description
Summary:Major ions and dissolved salts in syngenetic ice wedges in the 25–30 m thick Late Pleistocene Ledovy Obryv yedoma and the 60-m thick Ust'-Algan Obryv yedoma. Analysis of major ion chemistry of ice - titration methods (titrimetric methods) are based on determining the quantity of a reagent of known concentration that is required to react completely with the analyte.

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