T. Reiner et F. Arnold, LABORATORY INVESTIGATIONS OF GASEOUS SULFURIC-ACID FORMATION VIA SO3-]H2SO4+M - MEASUREMENT OF THE RATE-CONSTANT AND PRODUCT IDENTIFICATION(H2O+M), The Journal of chemical physics, 101(9), 1994, pp. 7399-7407
We have measured the reaction SO3+H2O+M-->H2SO4+M in a flow tube react
or in the pressure range between 31 and 260 mbar of synthetic air carr
ier gas. SO3 has been produced in the flow tube using a radical source
for production of OH, which was converted to SO3 by reaction with SO2
. The concentration of SO3 as well as the concentration of the reactio
n product has been measured by chemical ionization mass spectrometry (
CIMS). Evidence has been found for the product being H2SO4. With incre
asing H2O-concentration in the flow reactor, an exponential decrease o
f the concentration of SO3 accompanied by a corresponding rise of the
H2SO4-concentration has been observed. A detailed flow analysis has be
en carried out and the rate constants have been corrected for diffusiv
e effects. The effect of heterogeneous reactions on the flow reactor w
alls has been investigated and could partially be quantified. From the
experiment, values for the reaction rate constant in the range betwee
n 0.72 and 1.39 X 10(-15) cm(3) s(-1) have been inferred. These values
are thought to be due to gas phase reactions only. Within the experim
ental accuracy the reaction rate constant did not undergo a significan
t pressure variation. The mean rate constant averaged over the total p
ressure range is (1.2 +/- 0.2) x 10(-15) cm(3) s(-1).