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| Effect of OH scavengers on the chemical composition of α-pinene secondary organic aerosol
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| Role of sesquiterpenes in biogenic new particle formation
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| NO at low concentration can enhance the formation of highly oxygenated biogenic molecules in the atmosphere
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| High-frequency gaseous and particulate chemical characterization using extractive electrospray ionization mass spectrometry (Dual-Phase-EESI-TOF)
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| Survival of newly formed particles in haze conditions
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| Low‐volatility vapors and new particle formation over the Southern Ocean during the Antarctic Circumnavigation Expedition
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| Biogenic particles formed in the Himalaya as an important source of free tropospheric aerosols
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| Online monitoring of volatile organic compounds emitted from human bronchial epithelial cells as markers for oxidative stress
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| Large contribution to secondary organic aerosol from isoprene cloud chemistry
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| Effects of aerosol size and coating thickness on the molecular detection using extractive electrospray ionization
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| Photodegradation of <em>α</em>-pinene secondary organic aerosol dominated by moderately oxidized molecules
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| Molecular characterization of ultrafine particles using extractive electrospray time-of-flight mass spectrometry
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| Constraining the response factors of an extractive electrospray ionization mass spectrometer for near-molecular aerosol speciation
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| The driving factors of new particle formation and growth in the polluted boundary layer
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| Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions
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| Sources of particulate-matter air pollution and its oxidative potential in Europe
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| Oxidative stress-induced inflammation in susceptible airways by anthropogenic aerosol
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| On the fate of oxygenated organic molecules in atmospheric aerosol particles
Pospisilova, V., Lopez-Hilfiker, F. D., Bell, D. M., El Haddad, I., Mohr, C., Huang, W., … Slowik, J. G. (2020). On the fate of oxygenated organic molecules in atmospheric aerosol particles. Science Advances, 6(11), eaax8922 (11 pp.). https://doi.org/10.1126/sciadv.aax8922 |
| Rapid growth of new atmospheric particles by nitric acid and ammonia condensation
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