Mineralization and chemical composition of water-soluble salts in ice wedges, segregated texture-forming ice and ground ice in northern Siberia


Geochemical composition of Holocene syngenetic ice wedges of southern and central parts of the Yamal Peninsula (within the thick peat bogs in the Shchuchya River valley, the Seyakha settlement, the floodplain of the Lakkatoso River, and the vicinity of the Cape Kamenny settlement) was determined. The authors have analyzed the content of trace elements and heavy metals.Holocene ice wedges are ultra-fresh and fresh, their mineralization varies from 20 to 200 mg/l, hydrocarbonates and calcium dominate in the ion composition. Participation of chlorides in the ice wedges on terraces indicates the influence of marine aerosols, the same for the ice wedges on the floodplain means the direct participation water of Ob Bay in their formation. The increasing of iron ions in some fragments of ice wedges, comparable to their content in segregated ice in the peat bog, may indicate a periodic participation of swamp waters in the formation of ice wedges.

The mineralization and chemical composition of water-soluble salts in segregated ice and ice wedges were determined at the V.V. Dokuchaev Soil Science Institute.

DOI https://doi.org/10.1594/PANGAEA.937334
Related Identifier IsDocumentedBy https://doi.org/10.7256/2453-8922.2017.2.22980
Related Identifier IsDocumentedBy https://doi.org/10.7256/2453-8922.2018.3.27776
Related Identifier IsDocumentedBy https://doi.org/10.7256/2453-8922.2018.4.28583
Related Identifier IsDocumentedBy https://doi.org/10.7256/2453-8922.2016.2.21378
Related Identifier IsDocumentedBy https://doi.org/10.1016/j.grj.2016.09.002
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.937334
Creator Budantseva, Nadine A; Vasil'chuk, Yurij K ORCID logo
Publisher PANGAEA
Publication Year 2021
Funding Reference Russian Foundation for Basic Research https://doi.org/10.13039/501100002261 Crossref Funder ID 18-05-60272 Arctic; Russian Science Foundation https://doi.org/10.13039/501100006769 Crossref Funder ID 19-17-00126 https://rscf.ru/en/project/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
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Resource Type Dataset
Format text/tab-separated-values
Size 664 data points
Discipline Earth System Research
Spatial Coverage (67.764W, 67.457S, 73.579E, 70.167N); Yamal Peninsula, northwestern Siberia; Yamal-Nenets, Russia
Temporal Coverage Begin 1978-07-01T00:00:00Z
Temporal Coverage End 1997-07-31T00:00:00Z