2019
DOI: 10.3390/min9100627
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Potential for Mineral Carbonation of CO2 in Pleistocene Basaltic Rocks in Volos Region (Central Greece)

Abstract: Pleistocene alkaline basaltic lavas crop out in the region of Volos at the localities of Microthives and Porphyrio. Results from detailed petrographic study show porphyritic textures with varying porosity between 15% and 23%. Data from deep and shallow water samples were analysed and belong to the Ca-Mg-Na-HCO3-Cl and the Ca-Mg-HCO3 hydrochemical types. Irrigation wells have provided groundwater temperatures reaching up to ~30 °C. Water samples obtained from depths ranging between 170 and 250 m. The enhanced t… Show more

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Cited by 17 publications
(17 citation statements)
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“…The CarbFix procedure involves taking greenhouse gases from the geothermal steam and dissolving them in water under high pressure, then injecting them into porous basalt rock at a depth of 500 to 800 metres (Koukouzas et al 2019). The basalt acts like a sponge and captures CO2 for permanent storage in the ground.…”
Section: The Injection Processmentioning
confidence: 99%
See 1 more Smart Citation
“…The CarbFix procedure involves taking greenhouse gases from the geothermal steam and dissolving them in water under high pressure, then injecting them into porous basalt rock at a depth of 500 to 800 metres (Koukouzas et al 2019). The basalt acts like a sponge and captures CO2 for permanent storage in the ground.…”
Section: The Injection Processmentioning
confidence: 99%
“…Scientists have developed several other capture and storage procedures, with the German power market as an example (Spiecker et al 2014;Kelektsoglou 2018;Koukouzas et al 2009;McGrail et al 2006;Schaef et al 2010). These procedures help countries attract more investment (Kristjánsdóttir 2019a(Kristjánsdóttir , 2020 and become more competitive (Kristjánsdóttir 2017).…”
Section: Cost Structure Issues and Analysismentioning
confidence: 99%
“…At a given pH of formation brine, surface ionizable groups of silica will dissociate to a degree that is determined by temperature and salinity, producing predominantly negative surface charge density and potential, assuming pH conditions (near neutral- Kharaka et al (2006)) typical of sine aquifers. As injected and dissolved carbon dioxide dissociate into bicarbonate and hydrogen ions (Koukouzas et al, 2019) additional surface complexation based on hydrogen ion adsorption onto silica surface will proceed as:…”
Section: Surface Complexation and Charge Development In Geologic Systemsmentioning
confidence: 99%
“…At a given pH of formation brine, surface ionizable groups of silica will dissociate to a degree that is determined by temperature and salinity, producing predominantly negative surface charge density and potential, assuming pH conditions (near neutral-Kharaka et al 32 typical of sine aquifers. As injected and dissolved carbon dioxide dissociate into bicarbonate and hydrogen ions 77 additional surface complexation based on hydrogen ion adsorption onto silica surface will proceed as: …”
Section: Introductionmentioning
confidence: 99%