Kinetics of the IO Radical. 1. Reaction of IO with ClO
作者:Andrew A. Turnipseed、Mary K. Gilles、James B. Burkholder、A. R. Ravishankara
DOI:10.1021/jp970914g
日期:1997.7.1
The rate coefficient for the IO + ClO --> products (5) reaction was measured by coupling discharge flow and pulsed laser-induced fluorescence techniques. Rate coefficients were measured from 200 to 362 K by monitoring the temporal profile of IO in an excess of ClO The rate coefficient is described by the expression: k(5)(T) = (5.1 +/- 1.7) x 10-(12) exp[(280 +/- 80)/T] cm(3) molecule(-1) s(-1) where the quoted uncertainties include estimated systematic errors, Atomic iodine was identified as a major product of reaction 5. A branching ratio of Phi = 0.14 +/- 0.04 at 298 K was obtained for the sum of channels which do not produce I atoms.
Kinetics of the IO Radical. 2. Reaction of IO with BrO
作者:Mary K. Gilles、Andrew A. Turnipseed、James B. Burkholder,、A. R. Ravishankara、Susan Solomon
DOI:10.1021/jp9709159
日期:1997.7.1
The rate coefficient for the IO + BrO --> products (1) reaction was measured using pulsed laser photolysis with a discharge flow tube for radical production and pulsed laser-induced fluorescence and UV absorption for detection of IO and BrO radicals, respectively. Reaction 1 was studied under pseudo-first-order conditions in IO with an excess of BrO between 204 and 388 K at total pressures of 6-15 Torr. The Arrhenius expression obtained for non-iodine atom producing channels is k(la)(T) = (2.5 +/- 1.0) x 10(-11) exp[(260 +/- 100)/T] cm(3) molecule(-1) s(-1) independent of pressure. The rate coefficient for the reaction BrO + BrO --> products (2) and the UV absorption cross sections of BrO as a function of temperature were also determined as part of this study. The implications of these results to the loss rate of stratospheric ozone are discussed.