Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure

Natural gas hydrates form under low temperatures and high pressures. They can be found in abundance in permafrost environments and under the sea floor, where the temperature and pressure conditions ensure their stability. The conditions within petroleum transporting pipelines can enter the range of...

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Main Author: Tetlie, Emilie Sørfonden
Format: Master Thesis
Language:English
Published: The University of Bergen 2017
Subjects:
Online Access:https://hdl.handle.net/1956/17234
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author Tetlie, Emilie Sørfonden
author_facet Tetlie, Emilie Sørfonden
author_sort Tetlie, Emilie Sørfonden
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
description Natural gas hydrates form under low temperatures and high pressures. They can be found in abundance in permafrost environments and under the sea floor, where the temperature and pressure conditions ensure their stability. The conditions within petroleum transporting pipelines can enter the range of the hydrate stability zone which can result in formation of plugs. The understanding of formation and dissolution of hydrates is crucial for future production of hydrates and for hydrate inhibition within pipelines. At present there are no simple methods for examining hydrates within a porous medium. For further characterization of the formation and dissociation of hydrates within a porous medium, better methods are required. Magnetic resonance imaging (MRI) is applied as a tool for studying hydrates within porous media in this master thesis. The porous media used for this thesis was unconsolidated quartz sand. Magnetic resonance imaging detects the signals sent out by hydrogen nuclei after exposure of radio frequency waves. This technique provides the opportunity to create images from the inside of a porous medium, without cutting it open. The intensity response from hydrogen nuclei within THF hydrate samples has been used to estimate the hydrate saturation of these samples. The estimation of hydrate saturation has been performed both for the total sample and on a local scale simultaneously, by dividing the sample into several slices. The intensity response from the THF hydrate samples was also used to determine formation and dissociation patterns. The T2 relaxation process was studied during the dissociation and reforming of THF hydrates, both on a local scale and for the total sample. The possible effect of wettability preferences of a porous medium on the T2 relaxation process has also been considered. Masteroppgave i petroleumsteknologi PTEK399
format Master Thesis
genre permafrost
genre_facet permafrost
id ftunivbergen:oai:bora.uib.no:1956/17234
institution Open Polar
language English
op_collection_id ftunivbergen
op_relation https://hdl.handle.net/1956/17234
op_rights Copyright the Author. All rights reserved
publishDate 2017
publisher The University of Bergen
record_format openpolar
spelling ftunivbergen:oai:bora.uib.no:1956/17234 2025-01-17T00:17:08+00:00 Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure Tetlie, Emilie Sørfonden 2017-12-05T23:00:02Z application/pdf https://hdl.handle.net/1956/17234 eng eng The University of Bergen https://hdl.handle.net/1956/17234 Copyright the Author. All rights reserved THF THF Hydrates Hydrates MRI 752223 Master thesis 2017 ftunivbergen 2023-03-14T17:42:50Z Natural gas hydrates form under low temperatures and high pressures. They can be found in abundance in permafrost environments and under the sea floor, where the temperature and pressure conditions ensure their stability. The conditions within petroleum transporting pipelines can enter the range of the hydrate stability zone which can result in formation of plugs. The understanding of formation and dissolution of hydrates is crucial for future production of hydrates and for hydrate inhibition within pipelines. At present there are no simple methods for examining hydrates within a porous medium. For further characterization of the formation and dissociation of hydrates within a porous medium, better methods are required. Magnetic resonance imaging (MRI) is applied as a tool for studying hydrates within porous media in this master thesis. The porous media used for this thesis was unconsolidated quartz sand. Magnetic resonance imaging detects the signals sent out by hydrogen nuclei after exposure of radio frequency waves. This technique provides the opportunity to create images from the inside of a porous medium, without cutting it open. The intensity response from hydrogen nuclei within THF hydrate samples has been used to estimate the hydrate saturation of these samples. The estimation of hydrate saturation has been performed both for the total sample and on a local scale simultaneously, by dividing the sample into several slices. The intensity response from the THF hydrate samples was also used to determine formation and dissociation patterns. The T2 relaxation process was studied during the dissociation and reforming of THF hydrates, both on a local scale and for the total sample. The possible effect of wettability preferences of a porous medium on the T2 relaxation process has also been considered. Masteroppgave i petroleumsteknologi PTEK399 Master Thesis permafrost University of Bergen: Bergen Open Research Archive (BORA-UiB)
spellingShingle THF
THF Hydrates
Hydrates
MRI
752223
Tetlie, Emilie Sørfonden
Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title_full Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title_fullStr Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title_full_unstemmed Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title_short Application of MRI in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
title_sort application of mri in studies of tetrahydrofuran hydrates in quartz sand at atmospheric pressure
topic THF
THF Hydrates
Hydrates
MRI
752223
topic_facet THF
THF Hydrates
Hydrates
MRI
752223
url https://hdl.handle.net/1956/17234