The Earth's atmosphere is composed of an enormous variety of chemical species associated
with trace gases and aerosol particles whose composition and chemistry have critical …

Aromatic hydrocarbons (ArHCs) and oxygenated aromatic hydrocarbons (ArHC–OHs) are
emitted from a variety of anthropogenic activities and are important precursors of secondary …

Highly oxygenated organic molecules (HOMs) are important for the formation of secondary
organic aerosol (SOA), which poses serious health risks and exerts great influence on …

Dark chamber experiments were conducted to study the SOA formed from the oxidation of α-
pinene and Δ-carene under different peroxy radical (RO2) fate regimes: RO2+ NO3, RO2+ …

The quantification of an aerosol chemical composition is complicated by the uncertainty in
the sensitivity of each species detected. Soft-ionization response factors can vary widely …

Nighttime NO 3-initiated oxidation of biogenic volatile organic compounds (BVOCs) such as
monoterpenes is important for the atmospheric formation and growth of secondary organic …

Biogenic sources dominate annual emissions of volatile organic compounds (VOCs) to the
atmosphere. A large fraction of these are monoterpenes, which react with OH radicals, NO3 …

The reaction of α-pinene with NO 3 is an important sink of both α-pinene and NO 3 at night in
regions with mixed biogenic and anthropogenic emissions; however, there is debate on its …

Unsaturated alcohols are emitted in the atmosphere from anthropogenic and biological
sources. Although NO 3 radical-initiated reaction of unsaturated alcohols constitute a …

Night-time reactions of biogenic volatile organic compounds (BVOCs) and nitrate radicals
(NO 3) can lead to the formation of NO 3-initiated biogenic secondary organic aerosol …