Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology

To gain in-depth understanding of natural gas hydrate behavior it is necessary to identify key parameters that affect their formation, distribution and destabilization within sediments. Hydrate formation kinetics in porous media is amongst the aspects which deserve important considerations as it may...

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Published in:Fuel
Main Author: Ruffine, Livio
Format: Text
Language:English
Published: Elsevier Sci Ltd
Subjects:
geo
Online Access:https://doi.org/10.1016/j.fuel.2014.10.041
https://archimer.ifremer.fr/doc/00245/35580/34209.pdf
https://archimer.ifremer.fr/doc/00245/35580/
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spelling fttriple:oai:gotriple.eu:10670/1.0ox4y2 2023-05-15T17:11:43+02:00 Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology Ruffine, Livio https://doi.org/10.1016/j.fuel.2014.10.041 https://archimer.ifremer.fr/doc/00245/35580/34209.pdf https://archimer.ifremer.fr/doc/00245/35580/ en eng Elsevier Sci Ltd doi:10.1016/j.fuel.2014.10.041 10670/1.0ox4y2 https://archimer.ifremer.fr/doc/00245/35580/34209.pdf https://archimer.ifremer.fr/doc/00245/35580/ other Archimer, archive institutionnelle de l'Ifremer Fuel (0016-2361) (Elsevier Sci Ltd), 2015-02 , Vol. 141 , P. 173-184 geo envir Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ fttriple https://doi.org/10.1016/j.fuel.2014.10.041 2023-01-22T17:10:23Z To gain in-depth understanding of natural gas hydrate behavior it is necessary to identify key parameters that affect their formation, distribution and destabilization within sediments. Hydrate formation kinetics in porous media is amongst the aspects which deserve important considerations as it may provide useful information on the formation history and the formation mechanisms of natural gas hydrate accumulations. Yet, it is at its early stage. In this paper, experiments on methane hydrate formation and dissociation in porous media are reported and discussed. The first part of this work is devoted to the investigation of the kinetics of methane hydrate formation within silica sand using a custom-design apparatus. The latter is suitable for investigating small hydrate-bearing cores. The influence of the methane injection flow-rate is examined, and then a straightforward method is proposed to quantify the amount of hydrate-bound gas. In the second part, three mixtures of clays and sand are used as geologic matrix to study the influence of clay content on the hydrate morphology for a predetermined amount of injected water. Visual observations showed that the morphology shifts from disseminated through massive to moussy hydrates with increasing proportion of clays. Text Methane hydrate Unknown Fuel 141 173 184
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Ruffine, Livio
Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
topic_facet geo
envir
description To gain in-depth understanding of natural gas hydrate behavior it is necessary to identify key parameters that affect their formation, distribution and destabilization within sediments. Hydrate formation kinetics in porous media is amongst the aspects which deserve important considerations as it may provide useful information on the formation history and the formation mechanisms of natural gas hydrate accumulations. Yet, it is at its early stage. In this paper, experiments on methane hydrate formation and dissociation in porous media are reported and discussed. The first part of this work is devoted to the investigation of the kinetics of methane hydrate formation within silica sand using a custom-design apparatus. The latter is suitable for investigating small hydrate-bearing cores. The influence of the methane injection flow-rate is examined, and then a straightforward method is proposed to quantify the amount of hydrate-bound gas. In the second part, three mixtures of clays and sand are used as geologic matrix to study the influence of clay content on the hydrate morphology for a predetermined amount of injected water. Visual observations showed that the morphology shifts from disseminated through massive to moussy hydrates with increasing proportion of clays.
format Text
author Ruffine, Livio
author_facet Ruffine, Livio
author_sort Ruffine, Livio
title Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
title_short Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
title_full Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
title_fullStr Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
title_full_unstemmed Exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: Kinetic behavior and morphology
title_sort exploring methane-hydrate formation and dissociation in geologic materials through laboratory experiments: kinetic behavior and morphology
publisher Elsevier Sci Ltd
url https://doi.org/10.1016/j.fuel.2014.10.041
https://archimer.ifremer.fr/doc/00245/35580/34209.pdf
https://archimer.ifremer.fr/doc/00245/35580/
genre Methane hydrate
genre_facet Methane hydrate
op_source Archimer, archive institutionnelle de l'Ifremer
Fuel (0016-2361) (Elsevier Sci Ltd), 2015-02 , Vol. 141 , P. 173-184
op_relation doi:10.1016/j.fuel.2014.10.041
10670/1.0ox4y2
https://archimer.ifremer.fr/doc/00245/35580/34209.pdf
https://archimer.ifremer.fr/doc/00245/35580/
op_rights other
op_doi https://doi.org/10.1016/j.fuel.2014.10.041
container_title Fuel
container_volume 141
container_start_page 173
op_container_end_page 184
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