Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling

Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling

Salt migration may be another reason why pore-gas hydrates dissociate in permafrost, besides pressure and temperature changes. Temperature variations in frozen hydrate-saturated sediments interacting with a NaCl solution have been studied experimentally at a constant temperature, ~−6 °C typical for...

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Bibliographic Details
Main Authors:	Evgeny Chuvilin, Valentina Ekimova, Dinara Davletshina, Boris Bukhanov, Ekaterina Krivokhat, Vladimir Shilenkov
Format:	Article
Language:	English
Published:	MDPI AG 2022-06-01
Series:	Geosciences
Subjects:	permafrost gas hydrate frozen sediment salt migration temperature variation hydrate dissociation
Online Access:	https://www.mdpi.com/2076-3263/12/7/261

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