Organic peroxides (POs) are organic molecules with one or more peroxide (− O–O−)
functional groups. POs are commonly regarded as chemically labile termination products …

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

Atmospheric ice nucleating particles (INPs) influence global climate by altering cloud
formation, lifetime, and precipitation efficiency. The role of secondary organic aerosol (SOA) …

Organosulfates (OSs) are ubiquitous in the atmosphere and serve as important tracers for
secondary organic aerosols (SOAs). Despite intense research over the years, the …

Inorganic species always coexist with organic materials in atmospheric particles and may
influence the heterogeneous oxidation of organic aerosols. However, very limited studies …

Recent studies have shown that instantaneous gas-particle equilibrium partitioning
assumptions fail to predict SOA formation, even at high relative humidity (∼ 85%), and …

Organosulfates (OSs) could be potentially important compounds in marine organic aerosols,
while their formation in marine atmospheres is far from clear due to a lack of cruise …

Organosulfur compounds (OrgSs), especially organosulfates, have been widely reported to
be present in large quantities in particulate organic matter found in various atmospheric …

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

2-Methyltetrols and C5H10O3 compounds, referred to as “C5-alkene triols,” are chemical
tracers used to estimate isoprene-derived epoxydiol (IEPOX) contributions to atmospheric …