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Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Podborny, Yevgenij Ye; Chizhova, Julia N (2021): Chloride and sulfate ions in massive ice and its potential water sources (North West Siberia) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.938420

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Abstract:
Lenses of massive ground ice and cryopegs were found at different levels in Holocene deposits in the northeastern Yamal Peninsula. Massive ice, 7 to 9 m thick, occurs at the depth 12 m under the Seyakha (Mutnaya) River. Multistage massive ground ice (four lenses, 0.4 m thick and 8 m long) exists in Gyda terrace I. Cl⁻/SO4⁻² ratios, spore-pollen spectra, and the presence of algae have implications for the origin of the Sabettayakha massive ice of different types. Columnar brown ice formed by freezing of sand saturated with water of the Ob Gulf, monolith brown ice is a frozen lake talik, while ultra-fresh white ice originates from lake and stream waters. Massive ground ice occurs in pre-Quaternary consolidated deposits, as well as in Holocene and modern sediments.
Keyword(s):
cryopegs; Holocene; Holocene sea-level changes; massive ice; northern West Siberia; Permafrost; Permafrost temperature; Stable isotopes; stable isotopes of water; Yamal Peninsula
Related to:
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Podborny, Yevgenij Ye; Chizhova, Julia Nikolaevna (2016): Multistage Holocene massive ground ice in Northern West Siberia. Earth's Cryosphere, 20(1), 34-45
Further details:
Fotiev, S M (1999): Patterns in the formation of ion-salt composition in natural water of Yamal peninsula (in Russian). Earth's Cryosphere, 3(2), 40-65
Streletskaya, I O; Leibman, Marina O (2004): Cryogeochemical relationship of massive ground ice, cryopegs, and their host deposits in Central Yamal on the basis of major ion compositions. Earth's Cryosphere, 6(3), 15-24
Vasil'chuk, Alla Constantinovna; Vasil'chuk, Yurij K (2015): Engineering-geological and geochemical conditions of polygonal landscapes on the Belyy Island (the Kara Sea). Engineering Geology, 1, 50-65
Vasil'chuk, Yurij K; Budantseva, Nadine A; Vasil'chuk, Alla Constantinovna; Podborny, Yevgeny; Podborny, Yevgenij Ye; Sullina, A N; Chizhova, Julia Nikolaevna (2015): Multistage Holocene massive ice near the Sabettayaha River mouth, Yamal Peninsula. Earth's Cryosphere, 19(4), 36-47
Funding:
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: 70.673413 * Median Longitude: 70.531160 * South-bound Latitude: 66.622701 * West-bound Longitude: 68.410163 * North-bound Latitude: 73.519389 * East-bound Longitude: 73.466835
Event(s):
Belyy_Island * Latitude: 73.331722 * Longitude: 70.058861 * Location: Yamal Peninsula, northwestern Siberia
Kara_Sea * Latitude: 73.519389 * Longitude: 72.514512 * Location: Kara Sea
Naduiyakha_River * Latitude: 70.574677 * Longitude: 68.614414 * Location: Yamal-Nenets, Russia * Method/Device: Multiple investigations (MULT)
Comment:
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.
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 IDSample IDVasil'chuk, Yurij K
7Sample typeSamp typeVasil'chuk, Yurij K
8Reference/sourceReferenceVasil'chuk, Yurij K
9ChlorideCl-mg/lVasil'chuk, Yurij KIon chromatography Stayer (Akvilon)
10Sulfate[SO4]2-mg/lVasil'chuk, Yurij KIon chromatography Stayer (Akvilon)
11Chloride/sulfate ratioCl/[SO4]2-Vasil'chuk, Yurij KCalculated
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
154 data points

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