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: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
T
Online Access:https://doi.org/10.3390/en14196019
https://doaj.org/article/97b48896a5f3440faef1f0157e5a2da1
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spelling ftdoajarticles:oai:doaj.org/article:97b48896a5f3440faef1f0157e5a2da1 2023-05-15T17:12:03+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 2021-09-01T00:00:00Z https://doi.org/10.3390/en14196019 https://doaj.org/article/97b48896a5f3440faef1f0157e5a2da1 EN eng MDPI AG https://www.mdpi.com/1996-1073/14/19/6019 https://doaj.org/toc/1996-1073 doi:10.3390/en14196019 1996-1073 https://doaj.org/article/97b48896a5f3440faef1f0157e5a2da1 Energies, Vol 14, Iss 6019, p 6019 (2021) Caspian Sea geohazards gas hydrates methane methane hydrate systems thickness of hydrates stability zone Technology T article 2021 ftdoajarticles https://doi.org/10.3390/en14196019 2022-12-30T20:09:56Z 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. Article in Journal/Newspaper Methane hydrate Directory of Open Access Journals: DOAJ Articles Energies 14 19 6019
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Caspian Sea
geohazards
gas hydrates
methane
methane hydrate systems
thickness of hydrates stability zone
Technology
T
spellingShingle Caspian Sea
geohazards
gas hydrates
methane
methane hydrate systems
thickness of hydrates stability zone
Technology
T
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
Technology
T
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 Article in Journal/Newspaper
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 MDPI AG
publishDate 2021
url https://doi.org/10.3390/en14196019
https://doaj.org/article/97b48896a5f3440faef1f0157e5a2da1
genre Methane hydrate
genre_facet Methane hydrate
op_source Energies, Vol 14, Iss 6019, p 6019 (2021)
op_relation https://www.mdpi.com/1996-1073/14/19/6019
https://doaj.org/toc/1996-1073
doi:10.3390/en14196019
1996-1073
https://doaj.org/article/97b48896a5f3440faef1f0157e5a2da1
op_doi https://doi.org/10.3390/en14196019
container_title Energies
container_volume 14
container_issue 19
container_start_page 6019
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