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Journal article

THE DIRECT MEASUREMENT OF DISSOLUTION KINETICS AT THE CALCITE WATER INTERFACE

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

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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

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