Abstract. The formation of particles from precursor vapors is an important source of atmospheric aerosol. Research at the Cosmics Leaving OUtdoor Droplets (CLOUD) facility at CERN tries to elucidate which vapors are responsible for this new-particle formation, and how in detail it proceeds. Initial measurement campaigns at the CLOUD stainless-steel aerosol chamber focused on investigating particle formation from ammonia (NH 3 ) and sulfuric acid (H 2 SO 4 ). Experiments were conducted in the presence of water, ozone and sulfur dioxide. Contaminant trace gases were suppressed at the technological limit. For this study, we mapped out the compositions of small NH 3 -H 2 SO 4 clusters over a wide range of atmospherically relevant environmental conditions. We covered [NH 3 ] in the range from < 2 to 1400 pptv, [H 2 SO 4 ] from 3.3 × 10 6 to 1.4 × 10 9 cm −3 (0.1 to 56 pptv), and a temperature range from −25 to +20 • C. Negatively and positively charged clusters were directly measured by an atmospheric pressure interface time-of-flight (APi-TOF)Published by Copernicus Publications on behalf of the European Geosciences Union.
S. Schobesberger et al.: On the composition of ammonia-sulfuric-acid clustersmass spectrometer, as they initially formed from gas-phase NH 3 and H 2 SO 4 , and then grew to larger clusters containing more than 50 molecules of NH 3 and H 2 SO 4 , corresponding to mobility-equivalent diameters greater than 2 nm. Water molecules evaporate from these clusters during sampling and are not observed. We found that the composition of the NH 3 -H 2 SO 4 clusters is primarily determined by the ratio of gas-phase concentrations [NH 3 ] is mostly larger than 10. We compared our results from CLOUD with APi-TOF measurements of NH 3 -H 2 SO 4 anion clusters during new-particle formation in the Finnish boreal forest. However, the exact role of NH 3 -H 2 SO 4 clusters in boundary layer particle formation remains to be resolved.