## Abstract Laboratory measurements at low temperatures of the ozone absorption coefficient differences required in the standard spectroscopic measurement of atmospheric ozone are described. The measurements were made with a Dobson spectrophotometer and a quartzβiodine source. The results at the st
Specific method for the determination of ozone in the atmosphere
β Scribed by Sham L. Sachdev; J.P. Lodge Jr.; Philip W. West
- Publisher
- Elsevier Science
- Year
- 1972
- Tongue
- English
- Weight
- 555 KB
- Volume
- 58
- Category
- Article
- ISSN
- 0003-2670
No coin nor oath required. For personal study only.
β¦ Synopsis
Ozone is the principal oxidant in the photochemical smog and a detailed study of ozone toxicity in man has been-reported '. It is also considered to be the most damaging of all air pollutants affecting vegetation '. The natural occurrence of ozone and its formation in the urban atmospheres is well knownj.
Published methods for the determination of ozone involve a variety of analytical techniques such as chemical oxidation4-7, catalytic decomposition' '*I 2, absorption of ultraviolet light8-lo, of an olefinic bond1'-i8. chemiluminescence or fluorescence l 3.14, and cleavage Most of these methods are not specific for ozone, and they arc generally used for determinations of total oxidants. Others which are specific suffer from thedisadvantage that they arc complicated or require frequent calibration. Obviously the need for a simple, specific and reliable method for ozone is becoming critical.
The method presented here is based on the reaction of ozone with 4-allyl-2methoxyphenol (eugenol). This reaction has been found to be specific. Ozone preferentially attacks the olefinic bond in ally1 groups and releases formaldehyde.
Formaldehyde formed is determined by a slight modification of the West-Gaeke procedure' 9 for sulfur dioxide. EXPERIMENTAL Apparatus Gas samplerszO, midget impingers (MSA Catalog No. 46984). Air flow meters (Fisher and Porter Co., Catalog No. 450-015). Dyna-vat pump (Cole-Parmer, Catalog No. 7064). Beckman DB spectrophotometer.
π SIMILAR VOLUMES
## Abstract Ozonesonde ascents have shown that frequently the vertical distribution of the ozone in the stratosphere is very complicated with strong maxima and minima. Such a complicated distribution was not expected. In an attempt to find the cause of this highly laminated structure of the ozone,