Area of research
Atmospheric Science · Health, Toxicology and Mutagenesis
Research interest
Research interests include Aerosol, Chemistry, Sulfuric acid, Nucleation, Particle (ecology), and Cloud condensation nuclei.
Anthropogenic organic aerosol in Europe produced mainly through second-generation oxidation
Global variability in atmospheric new particle formation mechanisms
Substantial contribution of transported emissions to organic aerosol in Beijing
Intense formation of secondary ultrafine particles from Amazonian vegetation fires and their invigoration of deep clouds and precipitation
The impact of ammonia on particle formation in the Asian Tropopause Aerosol Layer
Ammonium CI-Orbitrap: a tool for characterizing the reactivity of oxygenated organic molecules
Increasing contribution of nighttime nitrogen chemistry to wintertime haze formation in Beijing observed during COVID-19 lockdowns
Iodine oxoacids enhance nucleation of sulfuric acid particles in the atmosphere
Molecular Understanding of the Enhancement in Organic Aerosol Mass at High Relative Humidity
NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere
Synergistic HNO3–H2SO4–NH3 upper tropospheric particle formation
High Gas-Phase Methanesulfonic Acid Production in the OH-Initiated Oxidation of Dimethyl Sulfide at Low Temperatures
The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source
The missing base molecules in atmospheric acid–base nucleation
The effect of COVID-19 restrictions on atmospheric new particle formation in Beijing
Role of iodine oxoacids in atmospheric aerosol nucleation
The Synergistic Role of Sulfuric Acid, Bases, and Oxidized Organics Governing New‐Particle Formation in Beijing
The driving factors of new particle formation and growth in the polluted boundary layer
Formation of condensable organic vapors from anthropogenic and biogenic volatile organic compounds (VOCs) is strongly perturbed by NO <sub> <i>x</i> </sub> in eastern China
Molecular Composition of Oxygenated Organic Molecules and Their Contributions to Organic Aerosol in Beijing
Rapid growth of new atmospheric particles by nitric acid and ammonia condensation
Molecular understanding of new-particle formation from <i>α</i> -pinene between −50 and +25 °C
Photo-oxidation of Aromatic Hydrocarbons Produces Low-Volatility Organic Compounds
Enhanced growth rate of atmospheric particles from sulfuric acid
High concentration of ultrafine particles in the Amazon free troposphere produced by organic new particle formation
Size-dependent influence of NO <sub>x</sub> on the growth rates of organic aerosol particles
Molecular understanding of the suppression of new-particle formation by isoprene
Cloud–Aerosol–Turbulence Interactions: Science Priorities and Concepts for a Large-Scale Laboratory Facility
Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol
Formation of Highly Oxygenated Organic Molecules from α-Pinene Ozonolysis: Chemical Characteristics, Mechanism, and Kinetic Model Development