ATMOSPHERIC CHEMISTRY OF 1,3,5-TRIOXANE - UV SPECTRA OF C-C3H5O3(CENTER-DOT) AND (C-C3H5O3)O-2(CENTER-DOT) RADICALS, KINETICS OF THE REACTIONS OF (C-C3H5O3)O-2(CENTER-DOT) RADICALS WITH NO AND NO2, AND ATMOSPHERIC FATE OF THE ALKOXY RADICAL (C-C3H5O3)O(CENTER-DOT)

Citation
J. Platz et al., ATMOSPHERIC CHEMISTRY OF 1,3,5-TRIOXANE - UV SPECTRA OF C-C3H5O3(CENTER-DOT) AND (C-C3H5O3)O-2(CENTER-DOT) RADICALS, KINETICS OF THE REACTIONS OF (C-C3H5O3)O-2(CENTER-DOT) RADICALS WITH NO AND NO2, AND ATMOSPHERIC FATE OF THE ALKOXY RADICAL (C-C3H5O3)O(CENTER-DOT), The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 102(25), 1998, pp. 4829-4838
Citations number
28
Categorie Soggetti
Chemistry Physical
ISSN journal
10895639
Volume
102
Issue
25
Year of publication
1998
Pages
4829 - 4838
Database
ISI
SICI code
1089-5639(1998)102:25<4829:ACO1-U>2.0.ZU;2-8
Abstract
A pulse radiolysis technique was used to measure the UV absorption spe ctra of c-C3H5O3(.) and (c-C3H5O3)O-2(.) radicals over the range 220-3 00 nm, with sigma(c-C3H5O3(.))(250) (nm) = (5.2 +/- 0.7) x 10(-18) and sigma((c-C3H5O3)O-2(.))(250) (nm) = (3.7 +/- 0.4) x 10(-18) cm(2) mol ecule(-1). The self-reaction rate constant for the c-C3H5O3(.) radical s, defined as d[c-C3H5O3(.)]/dt = 2k(4)[c-C3H5O3(.)](2) was k(4) = (3. 1 +/- 0.6) x 10(-11) cm(3) molecule(-1) s(-1). The rate constants for reactions of (c-C3H5O3)O-2(.) radicals with NO and NO2 were k(6) = (5. 8 +/- 1.4) x 10(-12) and k(7) = (1.1 +/- 0.2) x 10(-11) cm(3) molecule (-1) s(-1), respectively. The rate constants for the reaction of F ato ms with 1,3,5-trioxane and the reaction of c-C3H5O3(.) radicals with O -2 were k(3) = (1.1 +/- 0.4) x 10(-10) and k(2) = (7.4 +/- 1.1) x 10(- 12) cm(3) molecule(-1) s(-1), respectively. Relative rate techniques w ere used to measure the rate constants for the reactions of OH radical s and Cl atoms with 1,3,5-trioxane and Cl atoms with H(O)COCH2OC(O)H, k(20) = (6.0 +/- 1.0) x 10(-12), k(24) = (1.0 +/- 0.2) x 10(-10), and k(25) = (5.1 +/- 1.0) x 10(-13) cm(3) molecule(-1) s(-1), respectively . FTIR-smog chamber systems were used to show that the atmospheric fat e of the alkoxy radical (c-C3H5O3)O(.) is decomposition via C-O bond s cission leading to the formation of H(O)COCH2OC(O)H (methylene glycol diformate). The IR spectrum of the peroxynitrate (c-C3H5O3)O2NO2 is pr esented. The results are discussed with respect to the atmospheric che mistry of 1,3,5-trioxane.