Amm. Doherty et al., IS HYDRAZOIC ACID (HN3) AN INTERMEDIATE IN THE DESTRUCTION OF HYDRAZINE BY EXCESS NITROUS-ACID, Journal of the Chemical Society. Dalton transactions, (19), 1995, pp. 3103-3107
The kinetics of the decomposition of NH2N=NOH, the intermediate absorb
ing at 225 nm formed in the nitrous acid-hydrazine reaction have been
studied by stopped-flow spectrophotometry at acidities up to 1 mol dm(
-1) H+. A substantial amount of protonation occurs at high acidities,
and the pK(a) of NH3+N=NOH is 0.57. In excess hydrazine decomposition
occurs to form hydrazoic acid (HN3), but in excess nitrous acid a rapi
d second nitrosation occurs by a diffusion-controlled reaction between
NO+ and NH2N=NOH which can bypass this pathway, though the possibilit
y of some hydrazoic acid formation cannot be ruled out. Spectrophotome
tric evidence has been obtained for the formation of a relatively stab
le species, probably a very minor component, a product of the double-n
itrosation reaction.