Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions

Experimental studies on clay sample saturation by methane hydrates proved that clay particles play an important role in the hydrate accumulation and decomposition processes in sediments. Depending on water content, the same clay mineral can serve as inhibitor, neutral component and promoter of hydra...

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Main Author: Vladimir S. Yakushev
Format: Article
Language:English
Published: MDPI AG 2018-12-01
Series:Geosciences
Subjects:
Online Access:http://www.mdpi.com/2076-3263/9/1/13
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author Vladimir S. Yakushev
author_facet Vladimir S. Yakushev
author_sort Vladimir S. Yakushev
collection DOAJ
description Experimental studies on clay sample saturation by methane hydrates proved that clay particles play an important role in the hydrate accumulation and decomposition processes in sediments. Depending on water content, the same clay mineral can serve as inhibitor, neutral component and promoter of hydrate formation. Wet clay is a good mineral surface for hydrate formation, but clays represent the worst media for hydrate accumulation and existence. Nevertheless, there are many observations of hydrate presence in clay-containing sediments, especially offshore. Experimental modelling of metastable hydrate decomposition in sediment samples recovered from permafrost in “Yamal crater” in the Russian Arctic has shown that metastable hydrates located in frozen, salted clays can generate huge volumes of gas, even with a negligible (tenth and hundredth of a degree) temperature rise.
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spelling doaj.art-d05b4374dd824ea28addcc6bcfb923f12022-12-22T03:19:05ZengMDPI AGGeosciences2076-32632018-12-01911310.3390/geosciences9010013geosciences9010013Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic RegionsVladimir S. Yakushev0Department of Gas and Gas Condensate Field Development and Operation, Gubkin Russian State University of Oil and Gas (National Research University), 65, Leninsky Prospekt, 119991 Moscow, RussiaExperimental studies on clay sample saturation by methane hydrates proved that clay particles play an important role in the hydrate accumulation and decomposition processes in sediments. Depending on water content, the same clay mineral can serve as inhibitor, neutral component and promoter of hydrate formation. Wet clay is a good mineral surface for hydrate formation, but clays represent the worst media for hydrate accumulation and existence. Nevertheless, there are many observations of hydrate presence in clay-containing sediments, especially offshore. Experimental modelling of metastable hydrate decomposition in sediment samples recovered from permafrost in “Yamal crater” in the Russian Arctic has shown that metastable hydrates located in frozen, salted clays can generate huge volumes of gas, even with a negligible (tenth and hundredth of a degree) temperature rise.http://www.mdpi.com/2076-3263/9/1/13clays hydrate formationpermafrostrelic gas hydratesgas liberationstemperature change“permafrost pockmarks”
spellingShingle Vladimir S. Yakushev
Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
Geosciences
clays hydrate formation
permafrost
relic gas hydrates
gas liberations
temperature change
“permafrost pockmarks”
title Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
title_full Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
title_fullStr Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
title_full_unstemmed Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
title_short Experimental Modeling of Methane Hydrate Formation and Decomposition in Wet Heavy Clays in Arctic Regions
title_sort experimental modeling of methane hydrate formation and decomposition in wet heavy clays in arctic regions
topic clays hydrate formation
permafrost
relic gas hydrates
gas liberations
temperature change
“permafrost pockmarks”
url http://www.mdpi.com/2076-3263/9/1/13
work_keys_str_mv AT vladimirsyakushev experimentalmodelingofmethanehydrateformationanddecompositioninwetheavyclaysinarcticregions