Cited by 94CO2 Sequestration and Geologic InteractionsCarbon Dioxide Capture TechnologiesCarbon dioxide utilization in catalysis

Enhancing process kinetics for mineral carbon sequestration

Open access
Krevor, Samuel C., Lackner, Klaus S.·2009·Energy Procedia

Abstract

The current low-cost process for mineral carbonation involves the direct carbonation of a slurry of magnesium or calcium silicate mineral with supercritical CO2. The process is currently limited by the slow reaction kinetics of the carbonation reactions, and in particular the slow dissolution rates of the silicates in weakly acidic conditions. Enhancing the dissolution rate in weakly acidic conditions has been identified as one of the main opportunities for lowering the costs of a direct mineral carbonation process. Serpentine has been identified by its reactivity and abundance as a potential mineral for use in a mineral carbonation process. In this paper we discuss the results of dissolution experiments in which ground serpentine was reacted in weakly acidic aqueous systems containing NH4Cl, NaCl,, sodium citrate, sodium EDTA, sodium oxalate, and sodium acetate. All experiments are carried out at 120 ∘C and under 20 bars of CO2 in a batch autoclave. It was found that the sodium salts of citrate, oxalate, and EDTA significantly enhance the dissolution of serpentine under weakly acidic conditions.

Integrity signals

Registry

Crossref · 10.1016/j.egypro.2009.02.315

Cites

2 of 2 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • Organic acids and their anions may affect mineral weathering rates by changing the dissolution rate far from equilibrium, making aqueous complexes with aqueous metals that would otherwise inhibit rates, and changing ion speciation in solution.

    “Organic acids and their anions may affect mineral weathering rates by three possible mechanisms: (1) changing the dissolution rate far from equilibrium either decreasing solution pH or forming complexes with cations at the mineral surface, which provides a new parallel reaction mechanism for the detachment of material from the mineral surface; (2) ability to make aqueous complexes with aqueous”
  • The pH effect can be explained by sorption of protons on an oxide surface polarizing the metal-oxygen bonds, weakening the bonding with the underlying lattice.

    “The pH effect can be explained by the fact that sorption of protons on an oxide surface polarizes the metal-oxygen bonds, weakening the bonding with the underlying lattice.103”
  • Far from equilibrium, the dissolution rates of most silicate minerals increase exponentially with increasing hydrogen ion concentration (low pH) in solution.

    “Far from equilibrium, the dissolution rates of most silicate minerals increase exponentially with increasing hydrogen ion concentration (low pH) in solution.”

Cites

Flagged first, then by citations

Cited by

Sorted by citations

Authors
Krevor, S. C., & Lackner, K. S.
Affiliations
Columbia University (US)
Corresponding author
Krevor, Samuel C.
Venue
Energy Procedia
Publisher
Elsevier BV
Published
2009-02
Volume
1
Issue
1
Pages
4867-4871
ISSN
1876-6102 (ISSN-L)
OpenAlex
W2067550424
Cited by
94
References
2
Citations by year
2026: 6 · 2025: 11 · 2024: 3 · 2023: 5 · 2022: 4 · 2021: 2 · 2020: 4 · 2019: 4 · 2018: 4 · 2017: 3 · 2016: 3 · 2015: 6 · 2014: 9 · 2013: 8 · 2012: 11
FWCI
16.34
Type
conference paper
Language
en
Open access
Locations
Energy Procedia (publishedVersion, cc-by-nc-nd)
Topics
  • Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
  • Physical Sciences › Engineering › Mechanical Engineering › Carbon Dioxide Capture Technologies
  • Physical Sciences › Chemical Engineering › Process Chemistry and Technology › Carbon dioxide utilization in catalysis
Keywords
CO2 mineralization, serpentine, silicate dissolution, dissolution kinetics, supercritical carbon dioxide, chelating agents, sodium citrate, sodium EDTA, sodium oxalate, sodium acetate, magnesium silicate minerals, calcium silicate minerals, CO2 sequestration

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review