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Carbon Dioxide Storage Potential of Cenozoic Saline Aquifers in the South Yellow Sea Basin
Carbon dioxide (CO2) storage in underwater reservoirs is a valuable method of reducing carbon emissions. Saline aquifers such as those in the South Yellow Sea Basin (SYSB), China, have great potential for geological CO2 storage. Thus, we use the recommended calculation method of USDOE and a formatio...
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Published in: | Energies (Basel) 2023-02, Vol.16 (4), p.1578 |
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description | Carbon dioxide (CO2) storage in underwater reservoirs is a valuable method of reducing carbon emissions. Saline aquifers such as those in the South Yellow Sea Basin (SYSB), China, have great potential for geological CO2 storage. Thus, we use the recommended calculation method of USDOE and a formation volume model to determine the geological conditions for CO2 storage and estimate the CO2 storage capacity of the Cenozoic saline aquifers in the SYSB (depth: 800–3200 m). Overall, the SYSB exhibits weak fault activity and seismicity, medium and low geothermal fields, four types of source sandstone reservoir, and four sets of carbon reservoir–caprock assemblages developed from the Cenozoic strata, providing relatively good geological conditions for CO2 storage. The estimated capacity of the Cenozoic strata ranges from 39.59 Gt to 426.94 Gt (average: 155.25 Gt), indicating an extensive storage capacity that can meet the carbon sequestration needs of Shandong and Jiangsu Provinces for approximately 89 years. The Yantai Depression has a lower geothermal gradient and terrestrial heat, weaker seismic activity, and double the storage capacity of the Qingdao Depression, indicating that it is the most suitable area for Cenozoic CO2 storage in the SYSB, whereas the Laoshan Uplift is not suitable for storage. This study provides a scientific basis for the selection of offshore CO2 storage sites. |
doi_str_mv | 10.3390/en16041578 |
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Saline aquifers such as those in the South Yellow Sea Basin (SYSB), China, have great potential for geological CO2 storage. Thus, we use the recommended calculation method of USDOE and a formation volume model to determine the geological conditions for CO2 storage and estimate the CO2 storage capacity of the Cenozoic saline aquifers in the SYSB (depth: 800–3200 m). Overall, the SYSB exhibits weak fault activity and seismicity, medium and low geothermal fields, four types of source sandstone reservoir, and four sets of carbon reservoir–caprock assemblages developed from the Cenozoic strata, providing relatively good geological conditions for CO2 storage. The estimated capacity of the Cenozoic strata ranges from 39.59 Gt to 426.94 Gt (average: 155.25 Gt), indicating an extensive storage capacity that can meet the carbon sequestration needs of Shandong and Jiangsu Provinces for approximately 89 years. The Yantai Depression has a lower geothermal gradient and terrestrial heat, weaker seismic activity, and double the storage capacity of the Qingdao Depression, indicating that it is the most suitable area for Cenozoic CO2 storage in the SYSB, whereas the Laoshan Uplift is not suitable for storage. This study provides a scientific basis for the selection of offshore CO2 storage sites.</description><identifier>ISSN: 1996-1073</identifier><identifier>EISSN: 1996-1073</identifier><identifier>DOI: 10.3390/en16041578</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Agricultural production ; Aquifers ; Basins ; Carbon dioxide ; Carbon sequestration ; Cenozoic ; Emissions ; Geologic depressions ; geological storage ; Geology ; Provinces ; Reservoir storage ; Reservoirs ; saline aquifer ; Sandstone ; Seismic activity ; Seismicity ; sequestration ; South Yellow Sea Basin ; Storage capacity ; Underwater</subject><ispartof>Energies (Basel), 2023-02, Vol.16 (4), p.1578</ispartof><rights>COPYRIGHT 2023 MDPI AG</rights><rights>2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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-c359t-bfb59efa3731b88546972f901ca58c6fcaff72c79d74522f2725ec14dada4f8f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2779492213/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2779492213?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,25753,27924,27925,37012,44590,75126</link.rule.ids></links><search><creatorcontrib>Yuan, Yong</creatorcontrib><creatorcontrib>Wang, Jianqiang</creatorcontrib><creatorcontrib>Chen, Jianwen</creatorcontrib><creatorcontrib>Cao, Ke</creatorcontrib><creatorcontrib>Liang, Jie</creatorcontrib><creatorcontrib>Lan, Tianyu</creatorcontrib><creatorcontrib>Lu, Dongyu</creatorcontrib><creatorcontrib>Guo, Xudong</creatorcontrib><title>Carbon Dioxide Storage Potential of Cenozoic Saline Aquifers in the South Yellow Sea Basin</title><title>Energies (Basel)</title><description>Carbon dioxide (CO2) storage in underwater reservoirs is a valuable method of reducing carbon emissions. Saline aquifers such as those in the South Yellow Sea Basin (SYSB), China, have great potential for geological CO2 storage. Thus, we use the recommended calculation method of USDOE and a formation volume model to determine the geological conditions for CO2 storage and estimate the CO2 storage capacity of the Cenozoic saline aquifers in the SYSB (depth: 800–3200 m). Overall, the SYSB exhibits weak fault activity and seismicity, medium and low geothermal fields, four types of source sandstone reservoir, and four sets of carbon reservoir–caprock assemblages developed from the Cenozoic strata, providing relatively good geological conditions for CO2 storage. The estimated capacity of the Cenozoic strata ranges from 39.59 Gt to 426.94 Gt (average: 155.25 Gt), indicating an extensive storage capacity that can meet the carbon sequestration needs of Shandong and Jiangsu Provinces for approximately 89 years. The Yantai Depression has a lower geothermal gradient and terrestrial heat, weaker seismic activity, and double the storage capacity of the Qingdao Depression, indicating that it is the most suitable area for Cenozoic CO2 storage in the SYSB, whereas the Laoshan Uplift is not suitable for storage. This study provides a scientific basis for the selection of offshore CO2 storage sites.</description><subject>Agricultural production</subject><subject>Aquifers</subject><subject>Basins</subject><subject>Carbon dioxide</subject><subject>Carbon sequestration</subject><subject>Cenozoic</subject><subject>Emissions</subject><subject>Geologic depressions</subject><subject>geological storage</subject><subject>Geology</subject><subject>Provinces</subject><subject>Reservoir storage</subject><subject>Reservoirs</subject><subject>saline aquifer</subject><subject>Sandstone</subject><subject>Seismic activity</subject><subject>Seismicity</subject><subject>sequestration</subject><subject>South Yellow Sea Basin</subject><subject>Storage capacity</subject><subject>Underwater</subject><issn>1996-1073</issn><issn>1996-1073</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpNUU1rFEEQbcSAYc3FX9DgTdjYn9PTx3U1JhAwsHrQS1PbU73pZdKV9PTix6_PxBW16lDFo97jUY-xV1Kca-3FWyyyE0Za1z9jp9L7bimF08__21-ws2nai7m0llrrU_ZtDXVLhb_P9CMPyDeNKuyQ31DD0jKMnBJfY6FflCPfwJgL8tXDISesE8-Ft9uZRId2y7_iONJ3vkHg72DK5SU7STBOePZnLtiXiw-f15fL608fr9ar62XU1rflNm2txwTaabnte2s671TyQkawfexShJScis4PzlilknLKYpRmgAFM6pNesKuj7kCwD_c130H9GQhy-A1Q3QWoLccRQyeUkF7CYKU1ANr3GLV2MoqIg-3FrPX6qHVf6eGAUwt7OtQy2w_KOW-8UvPfFuz8eLWDWTSXRK1CnHvAuxypYMozvnJGSyNN90R4cyTEStNUMf21KUV4yi78y04_AuvCidA</recordid><startdate>20230201</startdate><enddate>20230201</enddate><creator>Yuan, Yong</creator><creator>Wang, Jianqiang</creator><creator>Chen, Jianwen</creator><creator>Cao, Ke</creator><creator>Liang, Jie</creator><creator>Lan, Tianyu</creator><creator>Lu, Dongyu</creator><creator>Guo, Xudong</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>DOA</scope></search><sort><creationdate>20230201</creationdate><title>Carbon Dioxide Storage Potential of Cenozoic Saline Aquifers in the South Yellow Sea Basin</title><author>Yuan, Yong ; 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Saline aquifers such as those in the South Yellow Sea Basin (SYSB), China, have great potential for geological CO2 storage. Thus, we use the recommended calculation method of USDOE and a formation volume model to determine the geological conditions for CO2 storage and estimate the CO2 storage capacity of the Cenozoic saline aquifers in the SYSB (depth: 800–3200 m). Overall, the SYSB exhibits weak fault activity and seismicity, medium and low geothermal fields, four types of source sandstone reservoir, and four sets of carbon reservoir–caprock assemblages developed from the Cenozoic strata, providing relatively good geological conditions for CO2 storage. The estimated capacity of the Cenozoic strata ranges from 39.59 Gt to 426.94 Gt (average: 155.25 Gt), indicating an extensive storage capacity that can meet the carbon sequestration needs of Shandong and Jiangsu Provinces for approximately 89 years. The Yantai Depression has a lower geothermal gradient and terrestrial heat, weaker seismic activity, and double the storage capacity of the Qingdao Depression, indicating that it is the most suitable area for Cenozoic CO2 storage in the SYSB, whereas the Laoshan Uplift is not suitable for storage. This study provides a scientific basis for the selection of offshore CO2 storage sites.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/en16041578</doi><oa>free_for_read</oa></addata></record> |
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subjects | Agricultural production Aquifers Basins Carbon dioxide Carbon sequestration Cenozoic Emissions Geologic depressions geological storage Geology Provinces Reservoir storage Reservoirs saline aquifer Sandstone Seismic activity Seismicity sequestration South Yellow Sea Basin Storage capacity Underwater |
title | Carbon Dioxide Storage Potential of Cenozoic Saline Aquifers in the South Yellow Sea Basin |
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