St. Arnold et al., ION CHEMISTRY RELEVANT FOR CHEMICAL-IONIZATION DETECTION OF SO3, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D7), 1995, pp. 14141-14146
Rate constants and products were measured for over 50 ion-molecule rea
ctions involving SO3 or ions formed from SO3. All negative ions studie
d reacted with SO3 at or near the collisional rate by a variety of pro
cesses including charge transfer, O- transfer, ligand exchange, and cl
ustering. Ambient negative ions tended to form SO4- or SO4- core ions.
A chemical ionization detection scheme for monitoring SO3 in the atmo
sphere is presented based on CO3-(H2O)(n=0-1) or NO3-(H2O)(n=0-1) as t
he primary ions. The proposed scheme can be used in conjunction with p
revious schemes for monitoring SO2 and H2SO4 concentrations to measure
all three gases simultaneously. The measurements also confirm that th
e ion chemistry used in separate studies to monitor the reaction of SO
3 with H2O is correct and rapid and that the reaction of SO3 with posi
tive ion water clusters does not contribute to H2SO4 production in the
atmosphere.