- Abstract:
- The dissolution of calcite in acidic waters is, under conditions of high mass transport, controlled by the first order heterogeneous reaction of H+ at the interface and not by diffusion as previously thought. The implications of this for lake liming strategies (aimed at countering the effects of "acid rain') are significant. -from Author
- Publication status:
- Published
- Publisher copy:
- 10.1111/j.1365-2427.1989.tb01101.x
-
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- Journal:
- FRESHWATER BIOLOGY
- Volume:
- 22
- Issue:
- 2
- Pages:
- 285-288
- Publication date:
- 1989-10-05
- DOI:
- EISSN:
-
1365-2427
- ISSN:
-
0046-5070
- URN:
-
uuid:7e503fc6-1c35-4ade-90f5-ba2ab585ea16
- Source identifiers:
-
43154
- Local pid:
- pubs:43154
- Language:
- English
- Copyright date:
- 1989
Journal article
THE DISSOLUTION OF CALCITE IN ACID WATERS - MASS-TRANSPORT VERSUS SURFACE CONTROL
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