2009
DOI: 10.1038/ngeo683
|View full text |Cite
|
Sign up to set email alerts
|

Permanent storage of carbon dioxide in geological reservoirs by mineral carbonation

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1

Citation Types

0
329
0
1

Year Published

2013
2013
2017
2017

Publication Types

Select...
7
3

Relationship

0
10

Authors

Journals

citations
Cited by 445 publications
(330 citation statements)
references
References 42 publications
0
329
0
1
Order By: Relevance
“…The reactivity of forsterite and its silicate alteration products has received increasing attention as a potential source material for the divalent cations required to carbonate CO 2 during carbon storage efforts (e.g. Giammar et al, 2005;Oelkers and Schott, 2005;Bearat et al, 2006;Matter et al, 2007;Oelkers et al, 2008;Dufaud et al, 2009;Prigiobbe et al, 2009;Matter and Kelemen, 2009;King et al, 2010;Daval et al, 2011;Guyot et al, 2011;Broecker, 2012;Kohler et al, 2013;Gislason and Oelkers, 2014;Sissmann et al, 2014). This interest has led to a large number of studies aimed at characterizing forsterite dissolution behavior and rates at various fluid compositions and temperatures (Luce et al, 1972;Sanemasa et al, 1972, Grandstaff, 1978, 1986, Murphy and Helgeson, 1987, 1989Blum andLasaga, 1988, Banfield et al, 1990;Walther, 1991, 1992;Casey and Westrich, 1992, Awad et al, 2000, Chen and Brantley, 2000, Rosso and Rimstidt, 2000, Pokrovsky and Schott, 2000a, 2000b, Oelkers, 2001b, Giammar et al, 2005, Hänchen et al, 2006, Olsen and Rimstidt, 2008Davis et al, 2009;Rimstidt et al, 2012;Olsson et al, 2012;Plümper et al, 201...…”
Section: Introductionmentioning
confidence: 99%
“…The reactivity of forsterite and its silicate alteration products has received increasing attention as a potential source material for the divalent cations required to carbonate CO 2 during carbon storage efforts (e.g. Giammar et al, 2005;Oelkers and Schott, 2005;Bearat et al, 2006;Matter et al, 2007;Oelkers et al, 2008;Dufaud et al, 2009;Prigiobbe et al, 2009;Matter and Kelemen, 2009;King et al, 2010;Daval et al, 2011;Guyot et al, 2011;Broecker, 2012;Kohler et al, 2013;Gislason and Oelkers, 2014;Sissmann et al, 2014). This interest has led to a large number of studies aimed at characterizing forsterite dissolution behavior and rates at various fluid compositions and temperatures (Luce et al, 1972;Sanemasa et al, 1972, Grandstaff, 1978, 1986, Murphy and Helgeson, 1987, 1989Blum andLasaga, 1988, Banfield et al, 1990;Walther, 1991, 1992;Casey and Westrich, 1992, Awad et al, 2000, Chen and Brantley, 2000, Rosso and Rimstidt, 2000, Pokrovsky and Schott, 2000a, 2000b, Oelkers, 2001b, Giammar et al, 2005, Hänchen et al, 2006, Olsen and Rimstidt, 2008Davis et al, 2009;Rimstidt et al, 2012;Olsson et al, 2012;Plümper et al, 201...…”
Section: Introductionmentioning
confidence: 99%
“…One proposed method, currently in the early stages of testing, involves the pumping of CO 2 -rich solutions down boreholes in to rock formations that contain silicate minerals with the requisite cations that are expected to undergo carbonation reactions. This is referred to as in situ CCSM and has been described by Kelemen and Matter (2009) and extensively studied by researches of CarbFix pilot project in Iceland (Gislason et al, 2010 and references therein).…”
Section: Fundamentals Of the Ccsm Processmentioning
confidence: 99%
“…Numerous studies have been published in the past on sequestering CO2 [1][2][3][4][5][6][7] along with different direct and indirect methods of reducing the overall CO2 emissions. Among the CO2 sequestration methods, mineral route of carbonation, especially of alkaline earth oxide bearing rocks, has proven to be an effective means [4,[8][9][10][11][12][13]. The high compressive and tensile strength of secondary carbonate rocks [14][15][16], formed as a result of mineral trapping, suggests the possibility of using mineral carbonation to form a sustainable binder for construction.…”
Section: Introductionmentioning
confidence: 99%