The reaction of SH radical with N2O was investigated by using two complemen
tary experimental methods: (a) a pulsed photolysis apparatus where SH was d
etected via laser-induced fluorescence and (b) a discharge flow tube where
SH was detected via chemical ionization mass spectrometry. The rate coeffic
ient for this reaction, k(1), was found to be less than 5 x 10(-16) cm(3) m
olecule(-1) s(-1) at 298 K, in contrast to the large value reported in the
literature [Ravichandran; et al. Chem. Phys. Lett. 1994, 217, 375-379]. Sec
ondary reactions were deduced to be unimportant in our system. Some possibl
e reasons for the previously reported high value are presented. The low val
ue of k(1) makes the oxidation of SH by N2O and removal of N2O by SH unimpo
rtant in the earth's atmosphere.