Journal article icon

Journal article

The solubility product controls the rate of calcite dissolution in pure water and seawater

Abstract:
The dissolution of calcite crystals into water is revealed to be under thermodynamic control such that the rate of dissolution is controlled by the rate of diffusion of ions from a saturated surface layer adjacent to the calcite surface.
Publication status:
Published
Peer review status:
Peer reviewed

Actions

Access Document

Files:
Publisher copy:
10.1039/d3sc04063a

Authors

More by this author
Institution:
University of Oxford
Role:
Author
ORCID:
0000-0001-8829-5883
More by this author
Institution:
University of Oxford
Role:
Author
More by this author
Role:
Author
ORCID:
0000-0001-7276-9319
More by this author
Institution:
University of Oxford
Role:
Author
ORCID:
0000-0001-9841-5041


More from this funder
Funder identifier:
10.13039/501100004211
Grant:
Monitoring Ocean Ecosystems


Publisher:
Royal Society of Chemistry
Journal:
Chemical Science More from this journal
Volume:
15
Issue:
7
Pages:
2464-2472
Publication date:
2024-02-14
DOI:
EISSN:
2041-6539
ISSN:
2041-6520


Language:
English
Keywords:
Pubs id:
1611863
Local pid:
pubs:1611863
Source identifiers:
W4390703203
Deposit date:
2026-06-05
ARK identifier:
This ORA record was generated from metadata provided by an external service. It has not been edited by the ORA Team.

Terms of use


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP