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Heavy-atom kinetic isotope effects and mechanism of the acid-catalyzed o-semidine and p-semidine rearrangements and disproportionation of 4,4'-dichlorohydrazobenzene

Thesis/Dissertation ·
OSTI ID:6855644
In acidic 60% dioxane solution at 0/sup 0/C, 4,4'-dichlorohydrazobenzene (14) underwent concurrent disproportionation to form p-chloroaniline and 4,4'-dichloroazobenzene and o- and p-semidine rearrangement. In the p-semidine rearrangement one of the chlorine atoms of 14 is displaced, in essence, as Cl/sup +/. This requires participation of a second molecule of 14 in a redox reaction. The overall fate of 14, therefore, was to give 11% of o- and 12% of p-semidine rearrangement (along with 12% of 4,4'-dichloroazobenzene), and 60% of disproportionation, which accounts for 95% of 14. Nitrogen and carbon kinetic isotope effects (KIE) were determined for each of these reactions, with the use of (/sup 15/N,/sup 15/N')14, (2-/sup 14/C)14,(4-/sup 14/C)14, and (4,4'-/sup 13/C/sub 2/)14. Isotope ratios were measured in the trifluoroacetyl derivatives with a combination of scintillation counting, whole-molecule-ion mass spectrometry (WMMS), and isotope-ratio mass spectrometry (IRMS), and in no care was a KIE other than unity obtained. These results show that o-semidine formation from 14 complies with the expectation that a (1,3)-sigmatropic shift should not be a concerted process. Although a concerted (1,5)-sigmatropic shift is possible, the p-semidine results suggest that the p-semidine rearrangement of 14 does not proceed by a concerted process. However, in this case, the relevant KIE are for a bond-forming reaction, so that a firm decision either for or against concertedness is not possible. Finally, the results indicate that disproportionation involves one (or both) of the two semidine rearrangement intermediates. The most likely one is that of the p-semidine rearrangement.
Research Organization:
Texas Tech Univ., Lubbock (USA)
OSTI ID:
6855644
Country of Publication:
United States
Language:
English