- Abstract:
- The rate laws describing the dissolution of calcite in aqueous solution under conditions of pH <4 and >7 are established, and, for the first time, it is shown that under conditions of high mass transport, the reaction of H+ with CaCO3 is controlled by a surface process rather than by the rate of convection/diffusion in the solution.
- Publication status:
- Published
- Publisher copy:
- 10.1039/c39890000249
-
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- Journal:
- JOURNAL OF THE CHEMICAL SOCIETY-CHEMICAL COMMUNICATIONS
- Issue:
- 4
- Pages:
- 249-251
- Publication date:
- 1989-02-15
- DOI:
- ISSN:
-
0022-4936
- URN:
-
uuid:8700ff7e-9953-4222-9ec6-42af2fa85d7f
- Source identifiers:
-
43224
- Local pid:
- pubs:43224
- Language:
- English
- Copyright date:
- 1989
Journal article
THE DIRECT MEASUREMENT OF DISSOLUTION KINETICS AT THE CALCITE WATER INTERFACE
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