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Nikita Tananaev

Biographic Data

ID7997727
NAMENikita Tananaev
GIVEN NAMESNikita
FAMILY NAMETananaev
SIGNATURETANANAEV N
AFFILIATIONSMelnikov Permafrost Institute of the Siberian Branch of the Russian Academy of Science
ORCID0000-0003-2997-0169
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2015
LATEST PUBLICATION YEAR2025
H-INDEX0
  • Microstructure and geochemical properties of modern and buried soils and hosting permafrost sediments of the Batagay retrogressive thaw slump

    Open Access•A V Lupachev, Nikita Tananaev et al.•ARTICLE•Quaternary Research•2025

    The paleopedology of the world’s largest retrogressive thaw slump, Batagay, is understudied. Micromorphological and geochemical analysis reveal the properties of th host sediments and major pedogenic features. Epigenetic soil profiles of Marine Oxygen Isotope Stage (MIS) 7 (or older) and 5e are clearly distinguished and well developed due to favorable bioclimatic conditions for pedogenesis, probably similar to modern ones. The oldest unit contain…

  • Permafrost hydrology in changing climatic conditions

    Open Access•D A Streletskiy, Nikita Tananaev et al.•ARTICLE•Environmental Research Letters•2015

    Role of changing climatic conditions on permafrost degradation and hydrology was investigated in the transition zone between the tundra and forest ecotones at the boundary of continuous and discontinuous permafrost of the lower Yenisei River. Three watersheds of various sizes were chosen to represent the characteristics of the regional landscape conditions. Samples of river flow, precipitation, snow cover, and permafrost ground ice were collected…

No prominent works on this page.

  • Permafrost hydrology in changing climatic conditions

    Open Access•D A Streletskiy, Nikita Tananaev et al.•ARTICLE•Environmental Research Letters•2015

    Role of changing climatic conditions on permafrost degradation and hydrology was investigated in the transition zone between the tundra and forest ecotones at the boundary of continuous and discontinuous permafrost of the lower Yenisei River. Three watersheds of various sizes were chosen to represent the characteristics of the regional landscape conditions. Samples of river flow, precipitation, snow cover, and permafrost ground ice were collected…

  • Microstructure and geochemical properties of modern and buried soils and hosting permafrost sediments of the Batagay retrogressive thaw slump

    Open Access•A V Lupachev, Nikita Tananaev et al.•ARTICLE•Quaternary Research•2025

    The paleopedology of the world’s largest retrogressive thaw slump, Batagay, is understudied. Micromorphological and geochemical analysis reveal the properties of th host sediments and major pedogenic features. Epigenetic soil profiles of Marine Oxygen Isotope Stage (MIS) 7 (or older) and 5e are clearly distinguished and well developed due to favorable bioclimatic conditions for pedogenesis, probably similar to modern ones. The oldest unit contain…

Geomorphology (2 works) · Permafrost (2 works) · Soil water (2 works) · Archaeology (1 work) · Arctic (1 work) · Arctic and Antarctic ice dynamics (1 work) · Cement (1 work) · Climate change and permafrost (1 work) · Cryospheric studies and observations (1 work) · Drainage basin (1 work)

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