Hydroxymethanesulfonate (HMS), a product of the heterogeneous reaction betw
een S(IV) and HCHO, was measured in atmospheric aerosol samples collected a
t two locations indicating it can exist outside of clouds. Sampling was per
formed through collection with filters and analysis using ion chromatograph
y with a treatment step to distinguish between HMS and uncomplexed S(IV). C
oncentrations of HMS were found to range from below the detection limit to
6.5 ng m(-3) for samples collected in central New Mexico in the summer and
around 30 ng m(-3) for two samples collected in Seattle, Washington in the
spring. Higher concentrations were associated with greater occurrence of cl
ouds, which is the presumed source of the HMS. In the samples collected in
Seattle, about half of the HMS was found associated with fine particles. In
the central New Mexico samples, molar ratios of HMS to sulfate in particul
ate matter were found to be less than 0.002 indicating that HMS was a minor
contributor of aerosol sulfur under the conditions of the measurements. (C
) 1999 Elsevier Science Ltd. All rights reserved.