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Models of talik, permafrost and gas hydrate histories - Beaufort Mackenzie Basin, Canada

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F15%3A00472570" target="_blank" >RIV/67985530:_____/15:00472570 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.3390/en8076738" target="_blank" >http://dx.doi.org/10.3390/en8076738</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3390/en8076738" target="_blank" >10.3390/en8076738</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Models of talik, permafrost and gas hydrate histories - Beaufort Mackenzie Basin, Canada

  • Original language description

    Models of talik, permafrost and gas hydrate (GH) histories below shallow lakes are investigated and compared to models of Beaufort Mackenzie Basin (BMB) GH occurrences to describe lacustrine inundation effects, which are compared against factors controlling the variations among Mackenzie Delta (MD) permafrost, GH and talik occurrence. Models using a 2-4 degrees C boundary temperature range indicate that geological setting, specifically underlying lithology and porosity, are the primary controls in talik formation below lakes. Below a lake of any size, where the underlying lithology is sandy it is practically impossible to produce a pervasive talik or to completely degrade significant GH accumulations in response to the boundary condition thermal effects alone. Models predict that talik formation is, in such cases, restricted to the upper few tens of meters below the lake. Permafrost degradation appears common where porosities are <40% and water bottom temperatures reach 2-4 degrees C, in both marine and lacustrine settings. Where porosities are higher a thin GH stability zone can persist, even where deep taliks have formed.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DC - Seismology, volcanology and Earth structure

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2015

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Energies

  • ISSN

    1996-1073

  • e-ISSN

  • Volume of the periodical

    8

  • Issue of the periodical within the volume

    7

  • Country of publishing house

    CH - SWITZERLAND

  • Number of pages

    27

  • Pages from-to

    6738-6764

  • UT code for WoS article

    000359897800026

  • EID of the result in the Scopus database

    2-s2.0-84939167853