Simulation of the Conditions for the Formation and Dissociation of Methane Hydrate over the Last 130 000 Years

The thermobaric conditions of the formation, stability, and dissociation of continental gas hydrates were determined by simulation of the thermal state of the permafrost. The calculations covered the period over the last 130 000 years, taking into account the various paleo-settings, including contin...

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Published in:Doklady earth sciences 2018-06, Vol.480 (2), p.826-830
Main Authors: Arzhanov, M. M., Malakhova, V. V., Mokhov, I. I.
Format: Article
Language:English
Subjects:
Computer simulation
Dissociation
Earth and Environmental Science
Earth Sciences
Fluxes
Gas hydrates
Geophysics
Geothermal energy
Glaciation
Glaciology
Hydrates
Mathematical analysis
Metastable state
Methane
Methane hydrate
Methane hydrates
Permafrost
Simulation
Stability
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description The thermobaric conditions of the formation, stability, and dissociation of continental gas hydrates were determined by simulation of the thermal state of the permafrost. The calculations covered the period over the last 130 000 years, taking into account the various paleo-settings, including continental glaciation, marine transgression, and high geothermal fluxes. According to the numerical calculations, relict gas hydrates may currently exist in the metastable state in the permafrost at depths of less than 100–150 m.
doi_str_mv 10.1134/S1028334X18060211
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source Springer Nature
subjects Computer simulation
Dissociation
Earth and Environmental Science
Earth Sciences
Fluxes
Gas hydrates
Geophysics
Geothermal energy
Glaciation
Glaciology
Hydrates
Mathematical analysis
Metastable state
Methane
Methane hydrate
Methane hydrates
Permafrost
Simulation
Stability
title Simulation of the Conditions for the Formation and Dissociation of Methane Hydrate over the Last 130 000 Years
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