Neutral molecular cluster formation of sulfuric acid dimethylamine observed in real time under atmospheric conditions

TL;DR

This study uses advanced chamber experiments to observe neutral sulfuric acid-dimethylamine clusters up to 2 nm, revealing their formation mechanisms and growth limitations under atmospheric conditions.

Contribution

It provides the first direct measurements of neutral SA-DMA clusters containing up to 14 SA and 16 DMA molecules, bridging molecular and particle perspectives of nucleation.

Findings

Neutral clusters form near the kinetic limit, limited only by collision rates.

Formation rates of larger particles are much lower due to coagulation and wall loss.

Particle formation rates cannot be solely explained by cluster evaporation or critical nucleus composition.

Abstract

For atmospheric sulfuric acid (SA) concentrations the presence of dimethylamine (DMA) at mixing ratios of several parts per trillion by volume can explain observed boundary layer new particle formation rates. However, the concentration and molecular composition of the neutral (uncharged) clusters have not been reported so far due to the lack of suitable instrumentation. Here we report on experiments from the Cosmics Leaving Outdoor Droplets chamber at the European Organization for Nuclear Research revealing the formation of neutral particles containing up to 14 SA and 16 DMA molecules, corresponding to a mobility diameter of about 2 nm, under atmospherically relevant conditions. These measurements bridge the gap between the molecular and particle perspectives of nucleation, revealing the fundamental processes involved in particle formation and growth. The neutral clusters are found to form at or close to the kinetic limit where particle formation is limited only by the collision rate of SA molecules. Even though the neutral particles are stable against evaporation from the SA dimer onward, the formation rates of particles at 1.7-nm size, which contain about 10 SA molecules, are up to 4 orders of magnitude smaller comparedwith those of the dimer due to coagulation and wall loss of particles before they reach 1.7 nm in diameter. This demonstrates that neither the atmospheric particle formation rate nor its dependence on SA can simply be interpreted in terms of cluster evaporation or the molecular composition of a critical nucleus.