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Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2021): Ion concentration, salinity and total dissolved solids (TDS) in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933098

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Abstract:
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.
Keyword(s):
Holocene; Ion concentrations; massive ice; pollen and spores; Sabettayakha River; stable isotope data; Yamal Peninsula
Related to:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2016): Holocene multistage massive ice, Sabettayakha river mouth, Yamal Peninsula, northwest Siberia. GeoResJ, 9-12, 54-66, https://doi.org/10.1016/j.grj.2016.09.002
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Chizhova, Julia N; Podborny, Yevgeny; Vasil'chuk, Jessica Yurevna (2021): Depth of massive ice bodies near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia. PANGAEA, https://doi.org/10.1594/PANGAEA.933097
Funding:
Russian Foundation for Basic Research, grant/award no. 18-05-60272: Arctic
Russian Science Foundation, grant/award no. 19-17-00126: Verification and validation of Late Pleistocene paleotemperature scenario based on the stable isotope data in syngenetic ice wedges in Siberia using independent paleoclimatic models
Coverage:
Median Latitude: 61.465450 * Median Longitude: 62.453814 * South-bound Latitude: 52.319423 * West-bound Longitude: 33.387228 * North-bound Latitude: 71.249246 * East-bound Longitude: 106.802626
Date/Time Start: 2015-02-03T00:00:00 * Date/Time End: 2015-02-03T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 9.20 m
Event(s):
Baikal_Lake * Latitude: 52.319423 * Longitude: 106.802626 * Location: Baikalsee, Irkutsk, Russia * Method/Device: Multiple investigations (MULT)
Moscow * Latitude: 55.705339 * Longitude: 37.517816 * Method/Device: Sampling by hand (HAND)
Sabettayakha_river * Latitude: 71.249246 * Longitude: 72.107585 * Location: Yamal Peninsula, northwestern Siberia * Method/Device: Multiple investigations (MULT)
Comment:
Cation and anion concentrations in the ice were measured immediately after the ice melted, in the Chemical-Analytical Centre of the Geographical Department of Lomonosov Moscow State University by ion chromatography "Stayer" with a conductivity detector. The limit for chloride ions is considered 0.02 μg/mL. The accuracy and precision over a wide concentration range, and total uncertainty (including random and systematic errors reported at the 95% confidence level) of anion and cation determinations were further estimated and the values were found to be sufficient for analysis of the ice.
Data was submitted and proofread by Yurij K Vasil'chuk and Lyubov Bludushkina at the faculty of Geography, department of Geochemistry of Landscapes and Geography of Soils, Lomonosov Moscow State University.
Funding was received from the Russian Science Foundation (Award nr. 19-17-00126, field research) and the Russian Foundation for Basic Research (Award nr. 18-05-60272, isotope analysis).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventVasil'chuk, Yurij K
2Latitude of eventLatitudeVasil'chuk, Yurij K
3Longitude of eventLongitudeVasil'chuk, Yurij K
4LocationLocationVasil'chuk, Yurij K
5Borehole numberHole nrVasil'chuk, Yurij K
6Sample typeSamp typeVasil'chuk, Yurij K
7DEPTH, sediment/rockDepth sedmVasil'chuk, Yurij KGeocode – from
8DEPTH, sediment/rockDepth sedmVasil'chuk, Yurij KGeocode – to
9Sample IDSample IDVasil'chuk, Yurij K
10DATE/TIMEDate/TimeVasil'chuk, Yurij KGeocode
11pHpHVasil'chuk, Yurij K
12SulfurSmg/lVasil'chuk, Yurij K
13Total dissolved solidsTDSµS/cmVasil'chuk, Yurij K
14Bicarbonate ion[HCO3]-%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
15Chloride ionCl-%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
16Sulfate[SO4]2-%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
17NitrateNO3%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
18Calcium ionCa2+%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
19Magnesium ionMg2+%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
20Sodium ionNa+%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
21Potassium ionK+%Vasil'chuk, Yurij KIon chromatography (Stayer, Akvilon, RF)eq
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
178 data points

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