Ion concentration, salinity and total dissolved solids (TDS) in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia

Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. Three boreholes (Nr 12, 17 and 42) were drilled within the Holocene lagoon-marine floodplain of the Ob Bay and the first lagoon-marine terrace near the Sabett...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Budantseva, Nadine A, Vasil'chuk, Alla Constantinovna, Chizhova, Julia N, Podborny, Yevgeny, Vasil'chuk, Jessica Yurevna
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Baikal_Lake
Baikalsee
Irkutsk
Russia
Bicarbonate ion
Borehole number
Calcium ion
Chloride ion
DATE/TIME
DEPTH
sediment/rock
Event label
HAND
Holocene
Ion chromatography (Stayer
Akvilon
RF)
Ion concentrations
Latitude of event
Location
Longitude of event
Magnesium ion
massive ice
Moscow
MULT
Multiple investigations
Nitrate
pH
pollen and spores
Potassium ion
Sabettayakha_river
Sabettayakha River
Sample ID
Sample type
Sampling by hand
Sodium ion
stable isotope data
Sulfate
Sulfur
Total dissolved solids
White_Sea
White Sea
Yamal Peninsula
northwestern Siberia
Ob' Bay
Sabettayakha
Gulf of Ob
Sea ice
Siberia
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.933098
https://doi.org/10.1594/PANGAEA.933098
Description
Summary:Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. Three boreholes (Nr 12, 17 and 42) were drilled within the Holocene lagoon-marine floodplain of the Ob Bay and the first lagoon-marine terrace near the Sabettayakha River mouth in winter 2014 using a light portable drill. The drilling retrieved a 12 cm diameter core in an almost undisturbed condition. Massive ice was sampled from these boreholes for isotope, chemical and palynologic analyses. The ion concentration (%-equivalent - %-eq), salinity (S) and total dissolved solids (TDS) concentration was determined in newly melted snow, lake ice, sea ice and sea water. A single series of geochemical analysis of massive ice with other cryospheric objects was carried out for more reliable comparison and correct interpretation of geochemical data.

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