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dc.contributor.authorGaleczka, I.
dc.contributor.authorWolff-Boenisch, Domenik
dc.contributor.authorGislason, S.
dc.contributor.editorUnknown
dc.date.accessioned2017-01-30T12:08:38Z
dc.date.available2017-01-30T12:08:38Z
dc.date.created2014-11-19T01:13:26Z
dc.date.issued2013
dc.identifier.citationGaleczka, I. and Wolff-Boenisch, D. and Gislason, S. 2013. Experimental studies of basalt-H2O-CO2 interaction with a high pressure column flow reactor: the mobility of metals, in Unknown (ed), 11th International Conference on Greenhouse Gas Control Technologies, GHGT-11, Nov 18 2012, pp. 5823-5833. Kyoto, Japan: Elsevier.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/18567
dc.description.abstract

Here, we report on the mobility of metals at the early stage of CO2 injection into basalt, before significant precipitation of secondary minerals. Short-lived pulses (50-100 hours) of CO2-charged water were injected into a high pressure column flow reactor filled with basaltic glass grains at 22°C, 8 MPa of total pressure and a velocity of 0.4 cm/min. The residence time of the water within the column ranged from 8 to 10 hours. The column was conditioned with pure water, resulting in alkaline outflow (pH ~9). The pH of the inlet CO2-charged water was ~3.2, and the lowest pH measured in the column was 4.5, after less than 10 hours of water/rock interaction. The dissolved metal concentrations and metals relative mobility increased dramatically during the CO2-pulses; more than 100 times for Sr, Fe, Al, Ca, Ba, Mn, and Mg. Of these elements, all but Al can bind with CO2 to form carbonate minerals. Only the dissolved Al, Fe, Mn and Cr concentrations exceeded allowable drinking water limits. After the CO2-pulses, all of the elemental concentrations decreased close-to or even below what was measured during the conditioning of the column. The pH never reached ~9 which was the initial pH before CO2-pulses.

dc.publisherElsevier
dc.relation.urihttp://www.sciencedirect.com/science/article/pii/S1876610213007480/pdf?md5=0f77c5ff85d7cec6824ae7cac596df63&pid=1-s2.0-S1876610213007480-main.pdf
dc.subjectelemental mobility
dc.subjecthigh pressure column flow reactor
dc.subjectmineral storage
dc.titleExperimental studies of basalt-H2O-CO2 interaction with a high pressure column flow reactor: the mobility of metals
dc.typeConference Paper
dcterms.source.volume37
dcterms.source.startPage5823
dcterms.source.endPage5833
dcterms.source.issn1876-6102
dcterms.source.titleEnergy Procedia 37
dcterms.source.seriesEnergy Procedia 37
dcterms.source.conference11th International Conference on Greenhouse Gas Control Technologies, GHGT-11
dcterms.source.conference-start-dateNov 18 2012
dcterms.source.conferencelocationKyoto, Japan
dcterms.source.placeNetherlands
curtin.accessStatusFulltext not available


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