Secondary organic aerosols (SOA) are crucial constitution of fine particulate matter (PM),
which are mainly derived from photochemical oxidation products of primary organic matter …

Highly oxygenated organic molecules (HOM) are found to play an important role in the
formation and growth of secondary organic aerosol (SOA). SOA is an important type of …

Wintertime meteorological conditions are usually unfavorable for ozone (O3) formation due
to weak solar irradiation and low temperature. Here, we observed a prominent wintertime O3 …

Oxidation of isoprene by nitrate radicals (NO3) or by hydroxyl radicals (OH) under high NOx
conditions forms a substantial amount of organonitrates (ONs). ONs impact NOx …

Isoprene and monoterpene emissions to the atmosphere are generally dominated by
biogenic sources. The oxidation of these compounds can lead to the production of …

Biomass burning (BB) is a major source of atmospheric fine carbonaceous aerosols, which
play a significant, yet uncertain, role in modulating the Earth's radiation balance. However …

Isoprene nitrates are important chemical species in the atmosphere which contribute to the
chemical cycles that form ozone and secondary organic aerosol (SOA) with implications for …

Furans are emitted to the atmosphere during biomass burning from the pyrolysis of
cellulose. They are one of the major contributing volatile organic compound (VOC) classes …

Biogenic secondary organic aerosol (BSOA) makes up a significant proportion of organic
aerosol, and its formation chemistry, composition, and physical properties can be influenced …

To investigate the sources and formation mechanism of oxidized organic nitrogen (OON),
field measurements of OON were conducted using an iodide-adduct chemical ionization …