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Journal ArticleDOI

Absorption Spectrum and Reaction Kinetics of the HO2 Radical in the Gas Phase

C. J. Hochanadel, +2 more
- 01 May 1972 - 
- Vol. 56, Iss: 9, pp 4426-4432
TLDR
In this paper, it was shown that HO2 radicals were produced in the gas phase by flash photolysis of water vapor (3%) in an atmosphere of hydrogen, helium, or argon containing ∼ 2% oxygen.
Abstract
HO2 radicals were produced in the gas phase by flash photolysis of water vapor (3%) in an atmosphere of hydrogen, helium, or argon containing ∼ 2% oxygen. Water is dissociated in the first continuum to H and OH, and O2 converts the H atoms to HO2. Hydrogen nearly doubles the amount of HO2 produced by converting OH to H. The absorption spectrum of HO2 is a broad band with a peak at 2050 A. The molar extinction coefficient, emax, based on measurement of the H2O2 formed in the hydrogen system, is 1770 ± 150 M−1· cm−1. The rate constant for the bimolecular combination reaction, HO2+HO2 → H2O2 + O2, was evaluated as 5.7 ± 0.5 × 109 M−1· sec−1 at 298°K and for the reaction HO2+OH→ H2O+O2, k = 1.2 ± 0.2 × 1011M−1. sec−1. From auxiliary measurements of the rate of O3 formation it was also found that, in the flash photolysis of O2 (2%) in H2, hot O atoms react with H2 to form OH and H which are then converted to HO2.

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Citations
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Journal ArticleDOI

Organic peroxy radicals: Kinetics, spectroscopy and tropospheric chemistry

TL;DR: A review of the state of the art in peroxy radical detection can be found in this article, where a number of experimental techniques have been used for the generation and detection of peroxy radicals and products of their reactions.
Journal ArticleDOI

Solar photo rates for planetary atmospheres and atmospheric pollutants

TL;DR: In this article, the rate coefficients and excess energies for dissociation, ionization, and dissociative ionization are presented for atomic and molecular species that have been identified or are suspected to exist in the atmospheres of planets, satellites (moons), comets, or as pollutants in the Earth atmosphere.
Journal ArticleDOI

Chlorofluoromethanes in the Environment

TL;DR: In this article, the photoprocesses of atmospheric chlorofluoromethanes, including their ultimate sinks, are studied. Butt et al. present a detailed study of the photodissociation process of chlorofluromethane.
Book ChapterDOI

Rate Coefficients in the C/H/O System

J. Warnatz
TL;DR: In this article, a critical survey of reaction rate coefficient data important in describing high-temperature combustion of H2, CO, and small hydrocarbons up to C4 is presented.
Journal ArticleDOI

A discussion of the chemistry of some minor constituents in the stratosphere and troposphere

TL;DR: In this article, a discussion is given of atmospheric reactions in the H2O−CH4−O2−O3−NO ≥ 3−NO fixme x system.
References
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Book

Combustion, Flames and Explosions of Gases

TL;DR: The second edition of this book has been in short supply for some time and the authors have decided in favor of a reprint of the book rather than an extensive revision at this time.
Journal ArticleDOI

The ultraviolet bands of OH Fundamental data

TL;DR: In this paper, a new survey of the infrared and visible-light bands of the Earth's ozone (OH) is presented, which is used for temperature measurements in flames and other combustion processes.
Journal ArticleDOI

Normal atmosphere: large radical and formaldehyde concentrations predicted.

TL;DR: A radical chain reaction is proposed for the rapid removal of carbon monoxide, leading to acarbon monoxide lifetime as low as 0.2 year in the surface atmosphere.
Journal ArticleDOI

Absorption Coefficients of Water Vapor in the Vacuum Ultraviolet

TL;DR: In this paper, the absorption coefficients of water vapor in the region 1060-1860A were obtained by a photoelectric method described previously, and the results showed that the absorption coefficient was between the values reported by two groups of investigators.
Journal ArticleDOI

Absorption Coefficient of Ozone in the Ultraviolet and Visible Regions

TL;DR: In this article, the absorption coefficients of ozone in the near ultraviolet from the overlapping region at 2000A up to about 3500A and in the visible from about 4000-7500A.
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