THE INHIBITION OF CALCITE DISSOLUTION PRECIPITATION - MG2+ CATIONS
The dissolution of calcite under conditions of high pH (8.0-9.0) is shown to be strongly inhibited by the presence of magnesium (Mg2+) cations. Channel flow cell measurements are used to deduce the appropriate rate law for dissolution and it is demonstrated that the inhibition arises from competitiv...
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| Formaat: | Journal article |
| Gepubliceerd in: |
1994
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