Abstract
La Mer and Greenspan's measurements (Trans. Faraday Soc., 1937, 33, 1266) on the rate of the water-catalysed decomposition of nitramide and new results on the hydrolysis of acetic anhydride in H2O-D2O mixtures are analysed in terms of the theory of H2O-D2O systems. The results are shown to bear a qualitative resemblance to the thermodynamic isotope effect on the ionic product of water in H2O-D2O mixtures. They can be quantitatively accounted for in terms of transition-state models, consistent with the conclusions of other mechanistic studies, in which there is an incipient charge separation similar to the complete charge-separation in ionised water.
| Original language | English |
|---|---|
| Pages (from-to) | 984-987 |
| Number of pages | 4 |
| Journal | Journal of the Chemical Society A: Inorganic, Physical, and Theoretical Chemistry |
| DOIs | |
| Publication status | Published - 1969 |
| Externally published | Yes |
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