Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea

The Caspian Sea is a region of active hydrocarbon production, where apart from conventional accumulations, gas hydrates (GH) are known to exist. GH are a potential future source of energy, however, currently they pose danger for development of conventional fields. The goal of this research was to de...

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Published in:Energies
Main Authors: Vasily Bogoyavlensky, Alisa Yanchevskaya, Aleksei Kishankov
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/en14196019
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spelling ftmdpi:oai:mdpi.com:/1996-1073/14/19/6019/ 2023-08-20T04:07:58+02:00 Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea Vasily Bogoyavlensky Alisa Yanchevskaya Aleksei Kishankov 2021-09-22 application/pdf https://doi.org/10.3390/en14196019 EN eng Multidisciplinary Digital Publishing Institute H: Geo-Energy https://dx.doi.org/10.3390/en14196019 https://creativecommons.org/licenses/by/4.0/ Energies; Volume 14; Issue 19; Pages: 6019 Caspian Sea geohazards gas hydrates methane methane hydrate systems thickness of hydrates stability zone thermobaric conditions numerical modeling Text 2021 ftmdpi https://doi.org/10.3390/en14196019 2023-08-01T02:45:39Z The Caspian Sea is a region of active hydrocarbon production, where apart from conventional accumulations, gas hydrates (GH) are known to exist. GH are a potential future source of energy, however, currently they pose danger for development of conventional fields. The goal of this research was to determine the area of GH distribution and thickness of their stability zone in the Caspian Sea using numerical modeling and to define how certain parameters affect the calculated thickness. As a result of the research, cartographic schemes were created for the South and Middle Caspian, where GH were predicted. For the South Caspian, conditions for methane hydrates formation exist at depths of more than 419–454 m, and for the Middle Caspian, more than 416–453 m. The maximal thicknesses of methane hydrates stability zones for the South Caspian can reach 900–956 m, and for the Middle Caspian, 226–676 m. Variations of parameters of seafloor depth, geothermal gradient and gas composition can significantly change the resulting thickness of GH stability zone. Text Methane hydrate MDPI Open Access Publishing Energies 14 19 6019
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Caspian Sea
geohazards
gas hydrates
methane
methane hydrate systems
thickness of hydrates stability zone
thermobaric conditions
numerical modeling
spellingShingle Caspian Sea
geohazards
gas hydrates
methane
methane hydrate systems
thickness of hydrates stability zone
thermobaric conditions
numerical modeling
Vasily Bogoyavlensky
Alisa Yanchevskaya
Aleksei Kishankov
Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
topic_facet Caspian Sea
geohazards
gas hydrates
methane
methane hydrate systems
thickness of hydrates stability zone
thermobaric conditions
numerical modeling
description The Caspian Sea is a region of active hydrocarbon production, where apart from conventional accumulations, gas hydrates (GH) are known to exist. GH are a potential future source of energy, however, currently they pose danger for development of conventional fields. The goal of this research was to determine the area of GH distribution and thickness of their stability zone in the Caspian Sea using numerical modeling and to define how certain parameters affect the calculated thickness. As a result of the research, cartographic schemes were created for the South and Middle Caspian, where GH were predicted. For the South Caspian, conditions for methane hydrates formation exist at depths of more than 419–454 m, and for the Middle Caspian, more than 416–453 m. The maximal thicknesses of methane hydrates stability zones for the South Caspian can reach 900–956 m, and for the Middle Caspian, 226–676 m. Variations of parameters of seafloor depth, geothermal gradient and gas composition can significantly change the resulting thickness of GH stability zone.
format Text
author Vasily Bogoyavlensky
Alisa Yanchevskaya
Aleksei Kishankov
author_facet Vasily Bogoyavlensky
Alisa Yanchevskaya
Aleksei Kishankov
author_sort Vasily Bogoyavlensky
title Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
title_short Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
title_full Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
title_fullStr Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
title_full_unstemmed Forecast of Distribution and Thickness of Gas Hydrate Stability Zone at the Bottom of the Caspian Sea
title_sort forecast of distribution and thickness of gas hydrate stability zone at the bottom of the caspian sea
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/en14196019
genre Methane hydrate
genre_facet Methane hydrate
op_source Energies; Volume 14; Issue 19; Pages: 6019
op_relation H: Geo-Energy
https://dx.doi.org/10.3390/en14196019
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/en14196019
container_title Energies
container_volume 14
container_issue 19
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