Df. Smith et al., MEASUREMENT OF ORGANIC ATMOSPHERIC TRANSFORMATION PRODUCTS BY GAS-CHROMATOGRAPHY, International journal of environmental analytical chemistry, 54(4), 1994, pp. 265-281
The photooxidation of hydrocarbons in the atmosphere leads to the form
ation of organic species which are typically more polar in character t
han the parent compounds. In recent years, detailed hydrocarbon measur
ements for C1 to C10 alkanes, alkenes, and aromatics in the atmosphere
have involved the use of deactivated canisters and gas chromatography
, similar to that described by EPA Method TO-14. However, quantitative
measurements of atmospheric polar organic compounds by this method ar
e unreliable. Work in this laboratory frequently involves the analysis
of sample mixtures from smog chambers that are used to simulate urban
atmospheres for studying the formation of ozone and other potentially
hazardous compounds. Over the past several years we have developed an
inert cryogenic sampling system and related GC methods for the analys
is of the photochemical mixtures which are sensitive, reproducible and
provide adequate separation for non-polar hydrocarbons and their pola
r transformation products. These improvements have allowed a number of
kinetic and mechanistic studies to be conducted, which in the past ha
ve only been possible using in-situ Fourier Transform Infrared Spectro
scopy. This paper describes the system development including current s
trengths and limitations as applicable to experimental programs requir
ing measurements of polar organic compounds at near-atmospheric concen
trations.