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...
Main Authors: | Evgeny Chuvilin, Dinara Davletshina, Boris Bukhanov, Aliya Mukhametdinova, Vladimir Istomin |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2022-11-01
|
Series: | Geosciences |
Subjects: | |
Online Access: | https://www.mdpi.com/2076-3263/12/11/419 |
Similar Items
-
Migration of Salt Ions in Frozen Hydrate-Saturated Sediments: Temperature and Chemistry Constraints
by: Evgeny Chuvilin, et al.
Published: (2022-07-01) -
Temperature Variation during Salt Migration in Frozen Hydrate-Bearing Sediments: Experimental Modeling
by: Evgeny Chuvilin, et al.
Published: (2022-06-01) -
Thermal Conductivity Variations in Frozen Hydrate-Bearing Sand upon Heating and Dissociation of Pore Gas Hydrate
by: Evgeny Chuvilin, et al.
Published: (2023-10-01) -
Formation and Accumulation of Pore Methane Hydrates in Permafrost: Experimental Modeling
by: Evgeny Chuvilin, et al.
Published: (2018-12-01) -
Dissociation and Self-Preservation of Gas Hydrates in Permafrost
by: Evgeny Chuvilin, et al.
Published: (2018-11-01)