Secondary aerosol formation promotes water uptake by organic-rich wildfire haze particles in equatorial Asia. Atmospheric Chemistry and Physics. 18(11):7781-7798.. 2018.
1-octanol-water partitioning as a classifier of water soluble organic matters: Implication for solubility distribution. Aerosol Science and Technology. 51(5):602-613.. 2017.
Light-Absorbing Brown Carbon Aerosol Constituents from Combustion of Indonesian Peat and Biomass. Environmental Science and Technology. 51(8):4415-4423.. 2017.
Temperature and burning history affect emissions of greenhouse gases and aerosol particles from tropical peatland fire. Journal of Geophysical Research: Atmospheres. 122:1218-1292.. 2017.
Water uptake by fresh Indonesian peat burning particles is limited by water-soluble organic matter. Atmospheric Chemistry and Physics. 17(18):11591-11604.. 2017.
Population exposure to hazardous air quality due to the 2015 fires in Equatorial Asia. Scientific Reports. 6. 2016.
Uptake and release of gaseous species accompanying the reactions of isoprene photo-oxidation products with sulfate particles. Physical Chemistry Chemical Physics. 18(3):1595-1600.. 2016.
Changing shapes and implied viscosities of suspended submicron particles. Atmospheric Chemistry And Physics. 15(14):7819-7829.. 2015.
Elemental composition of organic aerosol: the gap between ambient and laboratory measurements. Geophysical Research Letters. 42(10):4182–4189.. 2015.
Particle classification by the tandem differential mobility analyzer- particle mass analyzer system. Aerosol Science and Technology. 49(7):508-520.. 2015.
Phase and acidity regulate the production of secondary organic material from isoprene photooxidation. Physical Chemistry Chemical Physics. 17(8):5670-5678.. 2015.
Phase state and deliquescence hysteresis of ammonium sulfate seeded secondary organic aerosol. Aerosol Science and Technology. 49(7). 2015.
Submicron particle mass concentrations and sources in the Amazonian wet season (AMAZE-08). Atmospheric Chemistry and Physics. 15:3687–3701.. 2015.
Uptake of epoxydiol isomers accounts for half of the particle-phase material produced from isoprene photooxidation via the HO2 pathway. Environmental Science and Technology. 49(1):250–258.. 2015.
An analytic equation for the volume fraction of condensationally grown mixed particles and applications to secondary organic material produced in continuously mixed flow reactors. Aerosol Science and Technology. 48(8):803-812.. 2014.
Classifying organic materials by oxygen-to-carbon elemental ratio to predict the activation regime of cloud condensation nuclei (CCN).. Atmos. Chem. Phys.. 13:5309–5324.. 2013.
Phase Transitions and Phase Miscibility of Mixed Particles of Ammonium Sulfate, Toluene-Derived Secondary Organic Material, and Water. Journal of Physical Chemistry. 117:8895–8906.. 2013.
Viscosity of α-pinene secondary organic material and implications for particle growth and reactivity. Proc. Natl. Acad. Sci. USA... 2013.
Particle mass yield from b-caryophyllene ozonolysis. Atmos. Chem. Phys.. 12:3165-3179.. 2012.
Particle size distributions following condensational growth in continuous flow aerosol reactors as derived from residence time distributions: theoretical development and application to secondary organic aerosol. Aerosol. Sci. Technol.. 46:937-949.. 2012.
The phase of atmospheric organic particles affects their reactivity. Proc. Natl. Acad. Sci. USA.. 109:17354–17359.. 2012.
Using elemental ratios to predict the density of organic material composed of carbon, hydrogen, and oxygen. Environ. Sci. Technol. 46:787-794.. 2012.
Cloud condensation nuclei (CCN) activity and oxygen-to-carbon elemental ratios following thermodenuder treatment of organic particles grown by a-pinene ozonolysis. Phys. Chem. Chem. Phys. 13:14571–14583.. 2011.
Cloud condensation nuclei (CCN) from fresh and aged air pollution in the megacity region of Beijing. Atmos. Chem. Phys.. 11:11023-11039.. 2011.