2020
DOI: 10.1016/j.ijggc.2020.103165
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A review on CO2 leakage detection in shallow subsurface using geophysical surveys

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Cited by 9 publications
(6 citation statements)
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“…Monitoring tools evaluated in research GCS projects could become mature tools by the time the first large-scale GCS storage sites enter the post-injection phase. Examples of those include electrical resistivity tomography (ERT), electromagnetic (EM) methods (Girard et al, 2011;Carrigan et al, 2013;Schmidt-Hattenberger et al, 2016;Park et al, 2017;Caesary et al, 2020), gravity monitoring methods (Nooner et al, 2007;Alnes et al, 2008;Alnes et al, 2011;Dodds et al, 2013;Bonneville et al, 2021), and vertical seismic profiling (Hovorka et al, 2011;Coueslan et al, 2013;Daley et al, 2015;Gotz et al, 2014;Bauer et al, 2019;White, 2019;Popik et al, 2020). The diversity and availability of various monitoring tools highlight the importance of adopting a flexible approach during monitoring design that should be adapted as technology improves.…”
Section: Reservoir Monitoring: a Mature And Proven Suite Of Technologiesmentioning
confidence: 99%
“…Monitoring tools evaluated in research GCS projects could become mature tools by the time the first large-scale GCS storage sites enter the post-injection phase. Examples of those include electrical resistivity tomography (ERT), electromagnetic (EM) methods (Girard et al, 2011;Carrigan et al, 2013;Schmidt-Hattenberger et al, 2016;Park et al, 2017;Caesary et al, 2020), gravity monitoring methods (Nooner et al, 2007;Alnes et al, 2008;Alnes et al, 2011;Dodds et al, 2013;Bonneville et al, 2021), and vertical seismic profiling (Hovorka et al, 2011;Coueslan et al, 2013;Daley et al, 2015;Gotz et al, 2014;Bauer et al, 2019;White, 2019;Popik et al, 2020). The diversity and availability of various monitoring tools highlight the importance of adopting a flexible approach during monitoring design that should be adapted as technology improves.…”
Section: Reservoir Monitoring: a Mature And Proven Suite Of Technologiesmentioning
confidence: 99%
“…Overall, it is clear that rock surface chemistry is a key parameter which characterizes subsurface settings and associated fluid flow, for example, in volcanic studies, geothermal energy production, hydrocarbon production, seismoelectric responses, or salt water intrusion into drinking water reservoirs. , Moreover, and importantly, the rock surface charge is also related to rock wettability, which is a crucial factor in multiphase flow scenarios, for example, in CO 2 geo-sequestration, H 2 geo-storage, contaminant hydrology, or hydrocarbon production. ,โˆ’ One current key concern during CO 2 geo-sequestration is the possibility of CO 2 leakage into groundwater aquifers which leads to degradation of groundwater quality . Injection of CO 2 into aquifers creates an acidic subsurface resulting in the production of H + ions and thereby a reduction in pH .…”
Section: Discussionmentioning
confidence: 99%
“…40,92โˆ’94 One current key concern during CO 2 geo-sequestration is the possibility of CO 2 leakage into groundwater aquifers which leads to degradation of groundwater quality. 95 Injection of CO 2 into aquifers creates an acidic subsurface resulting in the production of H + ions and thereby a reduction in pH. 96 Geochemical reactions between the CO 2 -rich acidic brine and the rock surface are thus of utmost importance to a systematic understanding of the characteristics and the chemical reactions of the mineral subsurface in order to accurately predict reservoir behavior and optimize the various abovementioned processes (especially where acid is involved).…”
Section: Sioh Ohmentioning
confidence: 99%
“…์ง€๊ตฌ๋ฌผ๋ฆฌํƒ์‚ฌ ๋ฐฉ๋ฒ•์€ ๋น„ํŒŒ๊ดด์ ์œผ๋กœ ๋งค์งˆ์˜ ๋ฌผ์„ฑ์„ ํŒŒ์•… ํ•˜์—ฌ ๋งค์งˆ ๋‚ด๋ถ€๋ฅผ ํ‰๊ฐ€ํ•  ์ˆ˜ ์žˆ๋Š” ๊ฐ€์žฅ ํšจ์œจ์ ์ด๋ฉด์„œ๋„ ์  ํ•ฉํ•œ ๊ธฐ๋ฒ•์œผ๋กœ (Walton et al, 2015), ์‹œ์ถ”๊ณต ์กฐ์‚ฌ ๋“ฑ์˜ ์ง์ ‘ ํƒ์‚ฌ์— ๋น„ํ•ด ๊ฒฝ์ œ์ ์ด๋‹ค. ๋ฌผ๋ฆฌํƒ์‚ฌ๋Š” ์ „ํ†ต์ ์œผ๋กœ ์„์œ ๋‚˜ ์ง€ํ•˜์ˆ˜, ๊ด‘๋ฌผ ๋“ฑ์˜ ์ž์› ์กฐ์‚ฌ์— ํ™œ์šฉ๋˜์–ด ์™”์œผ๋ฉฐ(e.g., Daneshvar Saein et al, 2012;Watlet et al, 2018), ํ™˜๊ฒฝ ์˜ค ์—ผ ๋ฐ ์•ˆ์ „ ๋ถ„์•ผ(e.g., Castelluccio et al, 2018;Soupios et al, 2007)๋‚˜ CO 2 ์ง€์ค‘ ์ €์žฅ ๊ด€๋ จ ๋ถ„์•ผ(e.g., Lamert et al, 2012;Denchik et al, 2014;Caesary et al, 2020) ๋“ฑ์—์„œ๋„ ํ™œ๋ฐœํ•˜๊ฒŒ ์ ์šฉ๋˜๋ฉฐ ์‘์šฉ ๋ถ„์•ผ๊ฐ€ ๋„“์–ด์ง€๊ณ  ์žˆ๋‹ค. ์‹ฌ์ธต์ฒ˜๋ถ„์žฅ์ด๋‚˜ URL ๋‚ด๋ถ€ ํ˜น์€ ์ง€ํ‘œ๋ฉด์—์„œ๋„ ๋ฌผ๋ฆฌํƒ์‚ฌ ๋ฅผ ์ˆ˜ํ–‰ํ•จ์œผ๋กœ์จ ์‹œ์„ค์˜ ์•ˆ์ „์„ฑ ํ‰๊ฐ€ํ•˜๊ณ  ํ˜„์žฅ ์‹คํ—˜์„ ๋ชจ ๋‹ˆํ„ฐ๋งํ•  ์ˆ˜ ์žˆ์„ ๋ฟ๋งŒ ์•„๋‹ˆ๋ผ(e.g., Shigeta et al, 2003;Siren et al, 2015;Macy et al, 2012), ์ง€ํ•˜ ๋งค์งˆ์˜ ์•”๋ฐ˜ ๊ท  ์—ด๊ณผ ์ง€ํ•˜์ˆ˜ ๋ถ„ํฌ ์ •๋ณด, ๊ณตํ•™์  ๋ฐฉ๋ฒฝ ๋“ฑ์˜ ๊ตฌ์กฐ์ง€์งˆํ•™์ , ์ˆ˜ ๋ฆฌ์ง€์งˆํ•™์ , ์—ญํ•™์  ํŠน์„ฑ๋„ ํŒŒ์•…ํ•  ์ˆ˜๋„ ์žˆ๋‹ค(e.g., Maineult et al, 2013;Baek et al, 2017;Heikkinen et al, 2021).…”
Section: ์„œ ๋ก unclassified