Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone

Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolv...
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Gespeichert in:

Autor*in:	Julie K. Pearce [verfasserIn] Grant K. W. Dawson [verfasserIn] Silvano Sommacal [verfasserIn] Suzanne D. Golding [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	CO micro-CT sandstone reservoir mineral trapping produced water CO

Übergeordnetes Werk:	In: Energies - MDPI AG, 2008, 14(2021), 21, p 6998
Übergeordnetes Werk:	volume:14 ; year:2021 ; number:21, p 6998

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/en14216998

Katalog-ID:	DOAJ085577294

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allfields	10.3390/en14216998 doi (DE-627)DOAJ085577294 (DE-599)DOAJ01a861bef05949d6b417a1d6bccf8486 DE-627 ger DE-627 rakwb eng Julie K. Pearce verfasserin aut Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping. CO<sub<2</sub< storage micro-CT sandstone reservoir mineral trapping produced water CO<sub<2</sub<-water-rock reactions Technology T Grant K. W. Dawson verfasserin aut Silvano Sommacal verfasserin aut Suzanne D. Golding verfasserin aut In Energies MDPI AG, 2008 14(2021), 21, p 6998 (DE-627)572083742 (DE-600)2437446-5 19961073 nnns volume:14 year:2021 number:21, p 6998 https://doi.org/10.3390/en14216998 kostenfrei https://doaj.org/article/01a861bef05949d6b417a1d6bccf8486 kostenfrei https://www.mdpi.com/1996-1073/14/21/6998 kostenfrei https://doaj.org/toc/1996-1073 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 14 2021 21, p 6998
spelling	10.3390/en14216998 doi (DE-627)DOAJ085577294 (DE-599)DOAJ01a861bef05949d6b417a1d6bccf8486 DE-627 ger DE-627 rakwb eng Julie K. Pearce verfasserin aut Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping. CO<sub<2</sub< storage micro-CT sandstone reservoir mineral trapping produced water CO<sub<2</sub<-water-rock reactions Technology T Grant K. W. Dawson verfasserin aut Silvano Sommacal verfasserin aut Suzanne D. Golding verfasserin aut In Energies MDPI AG, 2008 14(2021), 21, p 6998 (DE-627)572083742 (DE-600)2437446-5 19961073 nnns volume:14 year:2021 number:21, p 6998 https://doi.org/10.3390/en14216998 kostenfrei https://doaj.org/article/01a861bef05949d6b417a1d6bccf8486 kostenfrei https://www.mdpi.com/1996-1073/14/21/6998 kostenfrei https://doaj.org/toc/1996-1073 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 14 2021 21, p 6998
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allfieldsGer	10.3390/en14216998 doi (DE-627)DOAJ085577294 (DE-599)DOAJ01a861bef05949d6b417a1d6bccf8486 DE-627 ger DE-627 rakwb eng Julie K. Pearce verfasserin aut Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping. CO<sub<2</sub< storage micro-CT sandstone reservoir mineral trapping produced water CO<sub<2</sub<-water-rock reactions Technology T Grant K. W. Dawson verfasserin aut Silvano Sommacal verfasserin aut Suzanne D. Golding verfasserin aut In Energies MDPI AG, 2008 14(2021), 21, p 6998 (DE-627)572083742 (DE-600)2437446-5 19961073 nnns volume:14 year:2021 number:21, p 6998 https://doi.org/10.3390/en14216998 kostenfrei https://doaj.org/article/01a861bef05949d6b417a1d6bccf8486 kostenfrei https://www.mdpi.com/1996-1073/14/21/6998 kostenfrei https://doaj.org/toc/1996-1073 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 14 2021 21, p 6998
allfieldsSound	10.3390/en14216998 doi (DE-627)DOAJ085577294 (DE-599)DOAJ01a861bef05949d6b417a1d6bccf8486 DE-627 ger DE-627 rakwb eng Julie K. Pearce verfasserin aut Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping. CO<sub<2</sub< storage micro-CT sandstone reservoir mineral trapping produced water CO<sub<2</sub<-water-rock reactions Technology T Grant K. W. Dawson verfasserin aut Silvano Sommacal verfasserin aut Suzanne D. Golding verfasserin aut In Energies MDPI AG, 2008 14(2021), 21, p 6998 (DE-627)572083742 (DE-600)2437446-5 19961073 nnns volume:14 year:2021 number:21, p 6998 https://doi.org/10.3390/en14216998 kostenfrei https://doaj.org/article/01a861bef05949d6b417a1d6bccf8486 kostenfrei https://www.mdpi.com/1996-1073/14/21/6998 kostenfrei https://doaj.org/toc/1996-1073 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 14 2021 21, p 6998
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author	Julie K. Pearce
spellingShingle	Julie K. Pearce misc CO<sub<2</sub< storage misc micro-CT misc sandstone reservoir misc mineral trapping misc produced water misc CO<sub<2</sub<-water-rock reactions misc Technology misc T Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone
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topic_title	Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone CO<sub<2</sub< storage micro-CT sandstone reservoir mineral trapping produced water CO<sub<2</sub<-water-rock reactions
topic	misc CO<sub<2</sub< storage misc micro-CT misc sandstone reservoir misc mineral trapping misc produced water misc CO<sub<2</sub<-water-rock reactions misc Technology misc T
topic_unstemmed	misc CO<sub<2</sub< storage misc micro-CT misc sandstone reservoir misc mineral trapping misc produced water misc CO<sub<2</sub<-water-rock reactions misc Technology misc T
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title	Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone
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title_full	Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone
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title_sort	micro ct and experimental study of carbonate precipitation from co<sub<2</sub< and produced water co-injection into sandstone
title_auth	Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone
abstract	Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping.
abstractGer	Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping.
abstract_unstemmed	Carbon dioxide geological storage involves injecting captured CO<sub<2</sub< streams into a suitable reservoir. Subsequent mineral trapping of the CO<sub<2</sub< as carbonate minerals is one of the most secure forms of trapping. Injection of CO<sub<2</sub< dissolved in water or co-injection of CO<sub<2</sub< with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO<sub<2</sub< could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO<sub<2</sub< storage was experimentally reacted with supercritical CO<sub<2</sub< and a synthetic produced water. Micro computed tomography (CT), QEMSCAN, and SEM were performed before and after the reaction. The sandstone sample was predominantly quartz with minor illite/muscovite and kaolinite. The sandstone sub-plug micro-CT porosity was 11.1% and 11.4% after the reaction. Dissolved Ca, Mg, and Sr decreased during the reaction. After the reaction with CO<sub<2</sub< and synthetic produced water, precipitation of crystalline carbonate minerals calcite and dolomite was observed in the pore space and on the rock surface. In addition, the movement of pore filling and bridging clays, as well as grains was observed. Co-injection of CO<sub<2</sub< with produced waters into suitable reservoirs has the potential to encourage CO<sub<2</sub< mineral trapping.
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title_short	Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone
url	https://doi.org/10.3390/en14216998 https://doaj.org/article/01a861bef05949d6b417a1d6bccf8486 https://www.mdpi.com/1996-1073/14/21/6998 https://doaj.org/toc/1996-1073
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Micro CT and Experimental Study of Carbonate Precipitation from CO<sub<2</sub< and Produced Water Co-Injection into Sandstone

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