Abstract
The position of equilibrium, with respect to nitrogen inversion, for cis-3,5-dimethylpiperidine (54% Ione pair axial, 46% Ione pair equatorial) was inferred from the proportions of configurations possessing [graphic omitted]–D (axial) and [graphic omitted]–D (equatorial) which were produced on mixing the amine with an excess of CF3·CO2D. The validity of the method was supported by experiments with model compounds, which showed (a) that exchange of H+(or D+) during the mixing period was relatively unimportant, and (b) that exchange of H+(or D+) in piperidine salts dissolved in CF3·CO2H (or CF3·CO2D) was exceptionally slow.