Theoretical and experimental investigations into the formation and accumulation of gas hydrates ...
The substantial volumes of gas hydrates found in the Arctic and in marine sediments are both a possible source of global climate change, and a potential future energy resource. The rate at which a hydrate layer forms, and the spatial distribution of hydrate in the layer are controlled by the physica...
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ftdatacite:10.14288/1.0053009 2024-04-28T08:10:25+00:00 Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... Rempel, Alan 2009 https://dx.doi.org/10.14288/1.0053009 https://doi.library.ubc.ca/10.14288/1.0053009 en eng University of British Columbia article-journal Text ScholarlyArticle 2009 ftdatacite https://doi.org/10.14288/1.0053009 2024-04-02T09:40:05Z The substantial volumes of gas hydrates found in the Arctic and in marine sediments are both a possible source of global climate change, and a potential future energy resource. The rate at which a hydrate layer forms, and the spatial distribution of hydrate in the layer are controlled by the physical conditions of the formation environment. To better understand the physical conditions that affect hydrate layer characteristics, I present a quantitative model for the formation of hydrates in a porous medium. The theory is tested using the the results of laboratory simulations of the modelled conditions. Conservation principles are used to derive the full set of governing equations using the minimum number of assumptions and simplifications. Scaling arguments, based on estimates of physical parameters in marine sediments, show that both heat and mass transport are dominated by diffusive processes, so advection may be neglected in most formation environments. Analytical solutions to the leading-order set of ... Text Arctic Climate change DataCite Metadata Store (German National Library of Science and Technology) |
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English |
description |
The substantial volumes of gas hydrates found in the Arctic and in marine sediments are both a possible source of global climate change, and a potential future energy resource. The rate at which a hydrate layer forms, and the spatial distribution of hydrate in the layer are controlled by the physical conditions of the formation environment. To better understand the physical conditions that affect hydrate layer characteristics, I present a quantitative model for the formation of hydrates in a porous medium. The theory is tested using the the results of laboratory simulations of the modelled conditions. Conservation principles are used to derive the full set of governing equations using the minimum number of assumptions and simplifications. Scaling arguments, based on estimates of physical parameters in marine sediments, show that both heat and mass transport are dominated by diffusive processes, so advection may be neglected in most formation environments. Analytical solutions to the leading-order set of ... |
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Text |
author |
Rempel, Alan |
spellingShingle |
Rempel, Alan Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
author_facet |
Rempel, Alan |
author_sort |
Rempel, Alan |
title |
Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
title_short |
Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
title_full |
Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
title_fullStr |
Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
title_full_unstemmed |
Theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
title_sort |
theoretical and experimental investigations into the formation and accumulation of gas hydrates ... |
publisher |
University of British Columbia |
publishDate |
2009 |
url |
https://dx.doi.org/10.14288/1.0053009 https://doi.library.ubc.ca/10.14288/1.0053009 |
genre |
Arctic Climate change |
genre_facet |
Arctic Climate change |
op_doi |
https://doi.org/10.14288/1.0053009 |
_version_ |
1797578307788603392 |