Determination of appropriate condition on replacing methane from hydrate with carbon dioxide

This paper is intended to determine the appropriate conditions for replacing CH(4) from NGH with CO(2). By analyzing the hydration equilibrium graphs and geotherms, the HSZs of NGH and CO(2) hydrate, both in permafrost and under deep sea, were determined. Based on the above analysis and experimental...

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Published in:Energy Conversion and Management
Main Authors: Zhou, Xitang, Fan, Shuanshi, Liang, Deqing, Du, Jianwei
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Ngh
Online Access:http://ir.giec.ac.cn/handle/344007/3460
http://www.sciencedirect.com/science/journal/01968904
https://doi.org/10.1016/j.enconman.2008.02.006
id ftchacadsciegiec:oai:ir.giec.ac.cn:344007/3460
record_format openpolar
spelling ftchacadsciegiec:oai:ir.giec.ac.cn:344007/3460 2024-09-15T18:30:03+00:00 Determination of appropriate condition on replacing methane from hydrate with carbon dioxide Zhou, Xitang Fan, Shuanshi Liang, Deqing Du, Jianwei 2008-08-01 http://ir.giec.ac.cn/handle/344007/3460 http://www.sciencedirect.com/science/journal/01968904 https://doi.org/10.1016/j.enconman.2008.02.006 英语 eng ENERGY CONVERSION AND MANAGEMENT Zhou, XT; Fan, SS; Liang, DQ; Du, JW.Determination of appropriate condition on replacing methane from hydrate with carbon dioxide,ENERGY CONVERSION AND MANAGEMENT,2008,49(8):2124-2129 http://ir.giec.ac.cn/handle/344007/3460 http://www.sciencedirect.com/science/journal/01968904 doi:10.1016/j.enconman.2008.02.006 Co(2) Ch(4) Ngh Replacement Appropriate Condition Science & Technology Physical Sciences Technology Thermodynamics Energy & Fuels Mechanics Physics LIQUID CO2 Nuclear Article 期刊论文 2008 ftchacadsciegiec https://doi.org/10.1016/j.enconman.2008.02.006 2024-07-26T05:27:20Z This paper is intended to determine the appropriate conditions for replacing CH(4) from NGH with CO(2). By analyzing the hydration equilibrium graphs and geotherms, the HSZs of NGH and CO(2) hydrate, both in permafrost and under deep sea, were determined. Based on the above analysis and experimental results, it is found that to replace CH(4) from NGH with gaseous CO(2), the appropriate experimental condition should be in the area surrounded by four curves: the geotherm, (H-V)(CO2), (L-V)(CO2) and (H-V)(CH4), and to replace CH4 from NGH with liquid CO(2), the condition should be in the area surrounded by three curves: (L-V)(CO2), (H-L)(CO2) and (H-V)CH4. For conditions in other areas, either CO(2) can not form a hydrate or CH4 can release little from its hydrate, which are not desirable results. (c) 2008 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper permafrost Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences: GIEC OpenIR Energy Conversion and Management 49 8 2124 2129
institution Open Polar
collection Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences: GIEC OpenIR
op_collection_id ftchacadsciegiec
language English
topic Co(2)
Ch(4)
Ngh
Replacement
Appropriate Condition
Science & Technology
Physical Sciences
Technology
Thermodynamics
Energy & Fuels
Mechanics
Physics
LIQUID CO2
Nuclear
spellingShingle Co(2)
Ch(4)
Ngh
Replacement
Appropriate Condition
Science & Technology
Physical Sciences
Technology
Thermodynamics
Energy & Fuels
Mechanics
Physics
LIQUID CO2
Nuclear
Zhou, Xitang
Fan, Shuanshi
Liang, Deqing
Du, Jianwei
Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
topic_facet Co(2)
Ch(4)
Ngh
Replacement
Appropriate Condition
Science & Technology
Physical Sciences
Technology
Thermodynamics
Energy & Fuels
Mechanics
Physics
LIQUID CO2
Nuclear
description This paper is intended to determine the appropriate conditions for replacing CH(4) from NGH with CO(2). By analyzing the hydration equilibrium graphs and geotherms, the HSZs of NGH and CO(2) hydrate, both in permafrost and under deep sea, were determined. Based on the above analysis and experimental results, it is found that to replace CH(4) from NGH with gaseous CO(2), the appropriate experimental condition should be in the area surrounded by four curves: the geotherm, (H-V)(CO2), (L-V)(CO2) and (H-V)(CH4), and to replace CH4 from NGH with liquid CO(2), the condition should be in the area surrounded by three curves: (L-V)(CO2), (H-L)(CO2) and (H-V)CH4. For conditions in other areas, either CO(2) can not form a hydrate or CH4 can release little from its hydrate, which are not desirable results. (c) 2008 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Zhou, Xitang
Fan, Shuanshi
Liang, Deqing
Du, Jianwei
author_facet Zhou, Xitang
Fan, Shuanshi
Liang, Deqing
Du, Jianwei
author_sort Zhou, Xitang
title Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
title_short Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
title_full Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
title_fullStr Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
title_full_unstemmed Determination of appropriate condition on replacing methane from hydrate with carbon dioxide
title_sort determination of appropriate condition on replacing methane from hydrate with carbon dioxide
publishDate 2008
url http://ir.giec.ac.cn/handle/344007/3460
http://www.sciencedirect.com/science/journal/01968904
https://doi.org/10.1016/j.enconman.2008.02.006
genre permafrost
genre_facet permafrost
op_relation ENERGY CONVERSION AND MANAGEMENT
Zhou, XT; Fan, SS; Liang, DQ; Du, JW.Determination of appropriate condition on replacing methane from hydrate with carbon dioxide,ENERGY CONVERSION AND MANAGEMENT,2008,49(8):2124-2129
http://ir.giec.ac.cn/handle/344007/3460
http://www.sciencedirect.com/science/journal/01968904
doi:10.1016/j.enconman.2008.02.006
op_doi https://doi.org/10.1016/j.enconman.2008.02.006
container_title Energy Conversion and Management
container_volume 49
container_issue 8
container_start_page 2124
op_container_end_page 2129
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