KINETIC-STUDY OF THE FORMATION OF ISOTOPICALLY SUBSTITUTED OZONE IN ARGON

Citation
J. Sehested et al., KINETIC-STUDY OF THE FORMATION OF ISOTOPICALLY SUBSTITUTED OZONE IN ARGON, J GEO RES-A, 103(D3), 1998, pp. 3545-3552
Citations number
34
Categorie Soggetti
Metereology & Atmospheric Sciences","Geosciences, Interdisciplinary","Astronomy & Astrophysics",Oceanografhy,"Geochemitry & Geophysics
Volume
103
Issue
D3
Year of publication
1998
Pages
3545 - 3552
Database
ISI
SICI code
Abstract
The kinetics of the formation of ozone was studied by using pulse radi olysis coupled with time-resolved UV absorption at 275 nm and at T = 2 94.9 +/- 0.6 K. The rate constant for the formation of ozone (OOO)-O-1 6-O-16-O-16 in argon was determined to be k(3a) = (3.38 +/- 0.04) x 10 (-34) cm(6) molecule(-2) s(-1). The rate constants for the reactions O -18 + (OO)-O-16-O-16 (k(3b)), O-16 + (OO)-O-16-O-18 (k(3c)), O-16 + (O O)-O-18-O-18 (k(3d)), O-18 + (OO)-O-16-O-18 (k(3e)), and O-18 + (OO)-O -18-O-18 (k(3f)) were studied, and the following parameters were deter mined: (k(3b) + k(3d))/(2k(3a)) = (1.184 +/- 0.037), (k(3c) + k(3e))/( 2k(3a)) = (1.155 +/- 0.062), and k(3f)/k(3a) = (0.977 +/- 0.021). The values for (k(3b) + k(3d))/(2k(3a)) and (k(3c) + k(3e))/(2k(3a)) obtai ned here are equal to the values derived from the product studies and the recently reported relative rate study but higher than the reported values for (k(3b) + k(3d))/(2k(3a)) and (k(3c) + k(3e))/(2k(3a)) Obta ined by using CO2 as a third body. The parameter k(3f)/k(3a) = (0.977 +/- 0.021) is lower than the value of k(3f)/k(3a) obtained by using CO 2 as a third body and the value derived from the product studies. Thes e different values of k(3f) may be partly due to changes in third body efficiency or due to resonance interactions between the excited ozone molecules and the third body. The absolute measurements reported here together with literature data suggest that the nature of the third bo dy is an important factor in controlling the enhancements of the rate constants for ozone formation and that asymmetry of neither ozone nor dioxygen ensure a fast ozone formation rate.