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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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 |
_version_ |
1766068801075412992 |