RECENT PROGRESS IN UNDERSTANDING PARTICLE NUCLEATION AND GROWTH

In the past half decade, several new tools have become available for i nvestigating particle nucleation and growth. A number of joint field a nd laboratory studies exploiting some of these new measurement capabil ities will be described and new insights shared. The ability to measur e OH, SO2, H2SO4 and aerosol number and size distributions has made po ssible a comparison between H2SO4 production and loss onto particles i n continental air masses. In regions remote from urban emissions, agre ement is typically quite good. In contrast, joint held measurements of nucleation precursors such as gas phase H2SO4 and ultrafine particles suggest that classical bimolecular nucleation theory may not properly describe the tropospheric nucleation process. An alternative mechanis m, possibly involving ammonia as a stabilizing agent for H2SO4/H2O mol ecular clusters is discussed. Finally, ultrafine particle measurements are shown to offer new opportunities for studying particle growth rat es. Preliminary results suggest that in a remote continental air mass, gas phase H2SO4 uptake is far too slow to explain observed growth rat es.