Jt. Jayne et al., PRESSURE AND TEMPERATURE-DEPENDENCE OF THE GAS-PHASE REACTION OF SO3 WITH H2O AND THE HETEROGENEOUS REACTION OF SO3 WITH H2O H2SO4 SURFACES/, The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 101(51), 1997, pp. 10000-10011
The gas-phase reaction of SO3 with H2O and the heterogeneous reaction
of SO3 with H2O-H2SO4 surfaces have been studied in a fast flow reacto
r coupled to a chemical ionization mass spectrometer (CIMS) for specie
s detection. The gas-phase reaction was studied under turbulent flow c
onditions over the pressure range from 100 to 760 Torr N-2 and the tem
perature range from 283 to 370 K. The loss rate of SO3 was measured un
der pseudo-first-order conditions; it exhibits a second-order dependen
ce on water vapor concentration and has a strong negative temperature
dependence. The first-order rate coefficient for the SO3 loss by gas-p
hase reaction shows no significant pressure dependence and can be expr
essed as k(1)(s(-1)) = 3.90 x 10(-41) exp(6830.6/T)[H2O](2) where [H2O
] is in units of molecule cm(-3) and T is in Kelvin. The overall uncer
tainty of our experimentally determined rate coefficients is estimated
to be +/-20%. At sufficiently low SO3 concentrations (<10(12) molecul
e cm(-3)) the rate coefficient is independent of the initial SO3 level
, as expected for a gas-phase reaction mechanism involving one SO3 and
two H2O molecules. However, at higher concentrations and lower temper
atures, increased rate coefficients were observed, indicating a fast h
eterogeneous reaction after the onset of binary homogeneous nucleation
of acid hydrate clusters leading to particle formation, which was ver
ified by light-scattering experiments. The heterogeneous loss of SO3 t
o the reactor walls has also been investigated under low pressure (1.1
-12.5 Torr) laminar flow conditions. The loss rate is highly dependent
on the humidity of the surface. In the presence of excess water the r
eactive sticking coefficient approaches unity and the wall loss rate i
s gas diffusion limited; under dry conditions it approaches zero, as e
xpected. The atmospheric implications of the homogeneous and heterogen
eous SO3-water reaction are discussed.