
Journal of Chemical Physics p. 5663 - 5669 (1988)
Update date:2022-08-16
Topics:
Matsuoka, Shingo
Nakamura, Hirone
Experiments were carried out using a time-resolved atmospheric pressure ionization mass- spectrometer (TRAPI) in N2-H2O (<*>1 ppm) system at temperatures from 233 to 543 K and at pressures from 167 to 760 Torr.The title reaction showed temperature and pressure dependences which were explained by the following scheme: N3+ + H2O<*>(N3+*H2O)* (forward and backward rate constants ka and kb; (N3+*H2O)*-->H2NO+ + N2 (forward rate constant kp; (N3+*H2O)* + N2-->H2NO+ + 2N2 (forward rate constant kd).Assuming that kd is equal to the collision rate constant of 7.1*10-10 cm3 s-1, the individual rate constants were determined as ka = 2.8*10-9 cm3 s-1 (302 K), kb = 17T3.6 s-1 where Tis temperature in K, and kp = 2.0*109 s-1 ( 302 K) .The product H2NO+ ion changed by successive reactions with H2O into H2NO+*H2O and subsequently to H3O+.
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