Organics enriched from samples of rain, snow, and
glacier ice were analyzed to determine the chemical
structure of the chloroorganic compounds that were most
abundant in such media. Gas chromatography with
atomic emission detection (GC-AED) was used to provide
an overview of the presence of volatile and extractable
chloroorganics at four sites in Europe and one site in
Antarctica. Real samples and isomer-specific standards
were then analyzed by gas chromatography with mass-spectrometric detection (GC-MS) to identify and confirm the
structure of the chloroorganics that had been detected
in the GC-AED analysis. The results revealed that of the
volatile chloroorganics found in the samples, dichloronitromethane, a compound not previously reported to occur
in the ambient environment, was often present in the
highest concentration (up to 130 ng L-1). Chlorobenzenes
were detected mainly as 1,4-dichlorobenzene and minor
amounts of 1,3- and 1,2-dichlorobenzene and one isomer of
tetrachlorobenzene (1,2,4,5- or 1,2,3,5-tetrachlorobenzene).
Chlorinated alkyl phosphates, which were normally
responsible for the largest peaks in the chlorine-specific
chromatograms of hexane- or ether-extractable compounds,
were present as tris(2-chloroethyl)phosphate, tris(1-chloro-2-propyl)phosphate, and one of the isomers bis(1-chloro-2-propyl)(3-chloro-1-propyl)phosphate or bis(1-chloro-2-propyl)(2-chloro-1-propyl)phosphate. All of the chloroorganic
compounds mentioned, i.e., dichloronitromethane,
chlorobenzenes, and chlorinated alkyl phosphates, were
detected at relatively remote sites in the northern hemisphere,
whereas only chlorobenzenes were found in a reference
sample of snow from Antarctica.