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
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Czech description
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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
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Result continuities
Project
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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
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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