Secondary organic aerosol (SOA) formed from the atmospheric oxidation of nonmethane organic gases (NMOG) is a major contributor to atmospheric aerosol mass. Emissions and smog chamber experiments were performed to investigate SOA formation from gasoline vehicles, diesel vehicles, and biomass burning. About 10-20
作者:Shantanu H, Jathar;Timothy D, Gordon;Christopher J, Hennigan;Havala O T, Pye;George, Pouliot;Peter J, Adams;Neil M, Donahue;Allen L, Robinson
来源:Proceedings of the National Academy of Sciences of the United States of America 2014 年 111卷 29期