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Enhanced carbon dioxide drainage observed in digital rock under intermediate wetting conditions
Carbon dioxide (CO 2 ) trapping in capillary networks of reservoir rocks is a pathway to long-term geological storage. At pore scale, CO 2 drainage displacement depends on injection pressure, temperature, and the rock’s interaction with the surrounding fluids. Modeling this interaction requires adeq...
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Published in: | Scientific reports 2024-07, Vol.14 (1), p.15852-11, Article 15852 |
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creator | Azpiroz, Jaione Tirapu Giro, Ronaldo Neumann Barros Ferreira, Rodrigo Nogueira Pereira da Silva, Marcio Fernandes Blanco Rodriguez, Manuela Lopez, Adolfo E. Correa Vasquez, David A. Lazo Esteves Ferreira, Matheus Del Grande, Mariana Ferreira Da Silva, Ademir Steiner, Mathias B. |
description | Carbon dioxide (CO
2
) trapping in capillary networks of reservoir rocks is a pathway to long-term geological storage. At pore scale, CO
2
drainage displacement depends on injection pressure, temperature, and the rock’s interaction with the surrounding fluids. Modeling this interaction requires adequate representations of both capillary volume and surface. For the lack of scalable representations, however, the prediction of a rock’s CO
2
storage potential has been challenging. Here, we report how to represent a rock’s pore space by statistically sampled capillary networks (ssCN) that preserve morphological rock characteristics. We have used the ssCN method to simulate CO
2
drainage within a representative sandstone sample at reservoir pressures and temperatures, exploring intermediate- and CO
2
-wet conditions. This wetting regime is often neglected, despite evidence of plausibility. By raising pressure and temperature we observe increasing CO
2
penetration within the capillary network. For contact angles approaching 90
∘
, the CO
2
saturation exhibits a pronounced maximum reaching 80
%
of the accessible pore volume. This is about twice as high as the saturation values reported previously. For enabling validation of our results and a broader application of our methodology, we have made available the rock tomography data, the digital rock computational workflows, and the ssCN models used in this study. |
doi_str_mv | 10.1038/s41598-024-65920-6 |
format | article |
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2
) trapping in capillary networks of reservoir rocks is a pathway to long-term geological storage. At pore scale, CO
2
drainage displacement depends on injection pressure, temperature, and the rock’s interaction with the surrounding fluids. Modeling this interaction requires adequate representations of both capillary volume and surface. For the lack of scalable representations, however, the prediction of a rock’s CO
2
storage potential has been challenging. Here, we report how to represent a rock’s pore space by statistically sampled capillary networks (ssCN) that preserve morphological rock characteristics. We have used the ssCN method to simulate CO
2
drainage within a representative sandstone sample at reservoir pressures and temperatures, exploring intermediate- and CO
2
-wet conditions. This wetting regime is often neglected, despite evidence of plausibility. By raising pressure and temperature we observe increasing CO
2
penetration within the capillary network. For contact angles approaching 90
∘
, the CO
2
saturation exhibits a pronounced maximum reaching 80
%
of the accessible pore volume. This is about twice as high as the saturation values reported previously. For enabling validation of our results and a broader application of our methodology, we have made available the rock tomography data, the digital rock computational workflows, and the ssCN models used in this study.</description><identifier>ISSN: 2045-2322</identifier><identifier>EISSN: 2045-2322</identifier><identifier>DOI: 10.1038/s41598-024-65920-6</identifier><identifier>PMID: 38982117</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>639/766/189 ; 704/106/694/682 ; 704/2151/2809 ; Carbon dioxide ; Drainage ; Humanities and Social Sciences ; multidisciplinary ; Physical characteristics ; Reservoirs ; Rocks ; Sandstone ; Science ; Science (multidisciplinary) ; Temperature requirements</subject><ispartof>Scientific reports, 2024-07, Vol.14 (1), p.15852-11, Article 15852</ispartof><rights>The Author(s) 2024</rights><rights>2024. The Author(s).</rights><rights>The Author(s) 2024. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c422t-95a2ba19fb2195405ce63a1cfee5ac7258182e77db90d6b4a2ba38cd3ef957af3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/3077590104/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/3077590104?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,25751,27922,27923,37010,37011,44588,53789,53791,74896</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/38982117$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Azpiroz, Jaione Tirapu</creatorcontrib><creatorcontrib>Giro, Ronaldo</creatorcontrib><creatorcontrib>Neumann Barros Ferreira, Rodrigo</creatorcontrib><creatorcontrib>Nogueira Pereira da Silva, Marcio</creatorcontrib><creatorcontrib>Fernandes Blanco Rodriguez, Manuela</creatorcontrib><creatorcontrib>Lopez, Adolfo E. Correa</creatorcontrib><creatorcontrib>Vasquez, David A. Lazo</creatorcontrib><creatorcontrib>Esteves Ferreira, Matheus</creatorcontrib><creatorcontrib>Del Grande, Mariana</creatorcontrib><creatorcontrib>Ferreira Da Silva, Ademir</creatorcontrib><creatorcontrib>Steiner, Mathias B.</creatorcontrib><title>Enhanced carbon dioxide drainage observed in digital rock under intermediate wetting conditions</title><title>Scientific reports</title><addtitle>Sci Rep</addtitle><addtitle>Sci Rep</addtitle><description>Carbon dioxide (CO
2
) trapping in capillary networks of reservoir rocks is a pathway to long-term geological storage. At pore scale, CO
2
drainage displacement depends on injection pressure, temperature, and the rock’s interaction with the surrounding fluids. Modeling this interaction requires adequate representations of both capillary volume and surface. For the lack of scalable representations, however, the prediction of a rock’s CO
2
storage potential has been challenging. Here, we report how to represent a rock’s pore space by statistically sampled capillary networks (ssCN) that preserve morphological rock characteristics. We have used the ssCN method to simulate CO
2
drainage within a representative sandstone sample at reservoir pressures and temperatures, exploring intermediate- and CO
2
-wet conditions. This wetting regime is often neglected, despite evidence of plausibility. By raising pressure and temperature we observe increasing CO
2
penetration within the capillary network. For contact angles approaching 90
∘
, the CO
2
saturation exhibits a pronounced maximum reaching 80
%
of the accessible pore volume. This is about twice as high as the saturation values reported previously. For enabling validation of our results and a broader application of our methodology, we have made available the rock tomography data, the digital rock computational workflows, and the ssCN models used in this study.</description><subject>639/766/189</subject><subject>704/106/694/682</subject><subject>704/2151/2809</subject><subject>Carbon dioxide</subject><subject>Drainage</subject><subject>Humanities and Social Sciences</subject><subject>multidisciplinary</subject><subject>Physical characteristics</subject><subject>Reservoirs</subject><subject>Rocks</subject><subject>Sandstone</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><subject>Temperature requirements</subject><issn>2045-2322</issn><issn>2045-2322</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNp9kk1vFSEUhomxsU3bP-DCTOLGzSifw7AypqnapImbdk0YODPlOhcqMK3-e7l3am1dyAZyznPew4EXodcEvyeY9R8yJ0L1Laa87YSiuO1eoCOKuWgpo_Tlk_MhOs15g-sSVHGiXqFD1queEiKPkD4PNyZYcI01aYihcT7-9A4al4wPZoImDhnSXQX8Ljn5YuYmRfu9WYKDVKMF0hacNwWaeyjFh6mxMThffAz5BB2MZs5w-rAfo-vP51dnX9vLb18uzj5dtpZTWlolDB0MUeNAiRIcCwsdM8SOAMJYSUVPegpSukFh1w18R7PeOgajEtKM7BhdrLoumo2-TX5r0i8djdf7QEyTNql4O4NWXNBxFD1IarmSYiACD4A7PkoQGEPV-rhq3S5DncxCKMnMz0SfZ4K_0VO804RQxoSUVeHdg0KKPxbIRW99tjDPJkBcsmZYSqXqVLiib_9BN3FJob7VnhIKE8wrRVfKpphzgvHxNgTrnR_06gdd_aD3ftBdLXrzdI7Hkj-_XwG2ArmmwgTpb-__yP4GEdrBzw</recordid><startdate>20240709</startdate><enddate>20240709</enddate><creator>Azpiroz, Jaione Tirapu</creator><creator>Giro, Ronaldo</creator><creator>Neumann Barros Ferreira, Rodrigo</creator><creator>Nogueira Pereira da Silva, Marcio</creator><creator>Fernandes Blanco Rodriguez, Manuela</creator><creator>Lopez, Adolfo E. 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Correa</au><au>Vasquez, David A. Lazo</au><au>Esteves Ferreira, Matheus</au><au>Del Grande, Mariana</au><au>Ferreira Da Silva, Ademir</au><au>Steiner, Mathias B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Enhanced carbon dioxide drainage observed in digital rock under intermediate wetting conditions</atitle><jtitle>Scientific reports</jtitle><stitle>Sci Rep</stitle><addtitle>Sci Rep</addtitle><date>2024-07-09</date><risdate>2024</risdate><volume>14</volume><issue>1</issue><spage>15852</spage><epage>11</epage><pages>15852-11</pages><artnum>15852</artnum><issn>2045-2322</issn><eissn>2045-2322</eissn><abstract>Carbon dioxide (CO
2
) trapping in capillary networks of reservoir rocks is a pathway to long-term geological storage. At pore scale, CO
2
drainage displacement depends on injection pressure, temperature, and the rock’s interaction with the surrounding fluids. Modeling this interaction requires adequate representations of both capillary volume and surface. For the lack of scalable representations, however, the prediction of a rock’s CO
2
storage potential has been challenging. Here, we report how to represent a rock’s pore space by statistically sampled capillary networks (ssCN) that preserve morphological rock characteristics. We have used the ssCN method to simulate CO
2
drainage within a representative sandstone sample at reservoir pressures and temperatures, exploring intermediate- and CO
2
-wet conditions. This wetting regime is often neglected, despite evidence of plausibility. By raising pressure and temperature we observe increasing CO
2
penetration within the capillary network. For contact angles approaching 90
∘
, the CO
2
saturation exhibits a pronounced maximum reaching 80
%
of the accessible pore volume. This is about twice as high as the saturation values reported previously. For enabling validation of our results and a broader application of our methodology, we have made available the rock tomography data, the digital rock computational workflows, and the ssCN models used in this study.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>38982117</pmid><doi>10.1038/s41598-024-65920-6</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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subjects | 639/766/189 704/106/694/682 704/2151/2809 Carbon dioxide Drainage Humanities and Social Sciences multidisciplinary Physical characteristics Reservoirs Rocks Sandstone Science Science (multidisciplinary) Temperature requirements |
title | Enhanced carbon dioxide drainage observed in digital rock under intermediate wetting conditions |
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