Formation of Metastability of Pore Gas Hydrates in Frozen Sediments: Experimental Evidence

Formation of Metastability of Pore Gas Hydrates in Frozen Sediments: Experimental Evidence

The Arctic permafrost and zones of hydrate stability may evolve to the conditions that allow gas hydrates to remain metastable for a long time due to self-preservation within 150 m depths. The behavior of relict (metastable) gas hydrates in frozen sediments is controlled externally by pressure and t...

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Autori principali: Evgeny Chuvilin, Dinara Davletshina, Boris Bukhanov, Aliya Mukhametdinova, Vladimir Istomin
Natura: Articolo
Lingua:English
Pubblicazione: MDPI AG 2022-11-01
Serie:Geosciences
Soggetti:
Arctic
permafrost
gas hydrate
experimental modelling
porous media
dissociation
Accesso online:https://www.mdpi.com/2076-3263/12/11/419

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https://www.mdpi.com/2076-3263/12/11/419

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