2011
DOI: 10.1016/j.ijggc.2011.01.006
|View full text |Cite
|
Sign up to set email alerts
|

Enhancing serpentine dissolution kinetics for mineral carbon dioxide sequestration

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

4
61
0
1

Year Published

2012
2012
2019
2019

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 112 publications
(66 citation statements)
references
References 37 publications
4
61
0
1
Order By: Relevance
“…The majority of previous research has focused on the aqueous carbonation of naturally occurring silicate minerals such as serpentine (Mckelvy et al, 2004;Alexander et al, 2007;Krevor and Lackner, 2011), olivine (Haug et al, 2010), limestone (Symonds et al, 2009) and wollastonite (Tai et al, 2006;Huijgen et al, 2006c;Daval et al, 2009) due to their high calcium or magnesium content. Although the CO 2 storage capacity of these natural Ca-Mg-silicate minerals is sufficient to fix the CO 2 emitted from the combustion of fossil fuels, the technological carbonation of these minerals is slow and energy demanding.…”
Section: Alkaline Wastes As Adsorbentsmentioning
confidence: 99%
See 1 more Smart Citation
“…The majority of previous research has focused on the aqueous carbonation of naturally occurring silicate minerals such as serpentine (Mckelvy et al, 2004;Alexander et al, 2007;Krevor and Lackner, 2011), olivine (Haug et al, 2010), limestone (Symonds et al, 2009) and wollastonite (Tai et al, 2006;Huijgen et al, 2006c;Daval et al, 2009) due to their high calcium or magnesium content. Although the CO 2 storage capacity of these natural Ca-Mg-silicate minerals is sufficient to fix the CO 2 emitted from the combustion of fossil fuels, the technological carbonation of these minerals is slow and energy demanding.…”
Section: Alkaline Wastes As Adsorbentsmentioning
confidence: 99%
“…Typical process conditions for the formation of magnesium carbonation via aqueous carbonation are p CO2 > 100 bar and a reaction time of hours (Huijgen et al, 2006c). However, MgCO 3 formation could be observed when natural ores (e.g., serpentine, olivine, etc) were selected as the feedstock for carbonation (Alexander et al, 2007;Krevor and Lackner, 2011). Furthermore, the study reported by Haug et al (2011) indicated that the mineral carbonation of olivine (generally rich in Mg contents) at 115 bar and 185°C is limited by MgCO 3 (magnesite) precipitation and not the olivine dissolution rate.…”
Section: Rate Of Carbonate Precipitationmentioning
confidence: 99%
“…Previous CCSM studies were performed under a wide range of physical and chemical conditions and mostly utilized only one type of serpentine, e.g. antigorite [Krevor and Lackner, 2011;Maroto-Valer et al, 2004;Park and Fan, 2004 and references therein]; lizardite [Daval et al, 2013;Sanna et al, 2013;Schulze et al, 2004;Wolf et al, 2004]; or chrysotile [Ryu et al, 2011;Rozalen et al, 2013]. Only a few have utilized two types of serpentine, lizardite and antigorite [O'Connor et al, 2002;Styles et al, 2014], and three or more have never been investigated under the same processing conditions, preventing a realistic comparison of the effects of mineral structure and composition on cation release; i.e.…”
Section: Introductionmentioning
confidence: 99%
“…Among the many materials tested, magnesium-rich materials are thought to be good candidates for carbonation due to their natural abundance [14] and relatively higher unit mass binding efficiency (e.g., as compared to calcium). For example, physical activation (grinding [15][16][17] or heating [18,19]), chemical leaching (acid [20][21][22], recyclable ammonium salt [23,24] or non-acidic ionic solutions [25]), bioleaching [26,27] were applied to Mg rich minerals to dissolve and concentrate Mg. However, the other CO 2 absorption and carbonate precipitation steps have been less explored.…”
Section: Co 2 Mineral Sequestrationmentioning
confidence: 99%