Major ions of Late Pleistocene massive ice exposed in lake Hanikosito (northern part) and Holocene ice wedges in the exposed outcrop on the terrace of Seyakha (Mutnaya) River

Total dissolved solids and major ions of the Late Pleistocene massive ice exposed in the northern part of the lake Hanikosito and Holocene ice wedges in the exposed outcrop on the terrace of Seyakha (Mutnaya) River, Bovanenkovskoye oil and gas condensate field.Concentrations of cations and anions in...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Budantseva, Nadine A, Vasil'chuk, Jessica Yurevna, Vasil'chuk, Alla Constantinovna, Garankina, Ekaterina Vadimovna, Chizhova, Julia Nikolaevna, Shorkunov, Il'ya Germanovich
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2020
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.921684
https://doi.pangaea.de/10.1594/PANGAEA.921684
Description
Summary:Total dissolved solids and major ions of the Late Pleistocene massive ice exposed in the northern part of the lake Hanikosito and Holocene ice wedges in the exposed outcrop on the terrace of Seyakha (Mutnaya) River, Bovanenkovskoye oil and gas condensate field.Concentrations of cations and anions in ice were measured at the chemical analytical center of the Faculty of Geography at Lomonosov Moscow State University using the ion chromatograph "Stayer". Analytical precision for chloride ions is 0.02 μg/ml, and less than 0.01 mg/l for other anions and cations.