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Effect of Ozone, Clothing, Temperature, and Humidity on the Total OH Reactivity Emitted from Humans

MPG-Autoren
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Zannoni,  Nora
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Li,  Mengze
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Wang,  Nijing
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Ernle,  Lisa
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Williams,  Jonathan
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Zitation

Zannoni, N., Li, M., Wang, N., Ernle, L., Bekö, G., Wargocki, P., et al. (2021). Effect of Ozone, Clothing, Temperature, and Humidity on the Total OH Reactivity Emitted from Humans. Environmental Science & Technology, 55(20), 13614-13624. doi:10.1021/acs.est.1c01831.


Zitierlink: https://hdl.handle.net/21.11116/0000-0009-BB23-D
Zusammenfassung
People influence indoor air chemistry through their chemical emissions via breath and skin. Previous studies showed that direct measurement of total OH reactivity of human emissions matched that calculated from parallel measurements of volatile organic compounds (VOCs) from breath, skin, and the whole body. In this study, we determined, with direct measurements from two independent groups of four adult volunteers, the effect of indoor temperature and humidity, clothing coverage (amount of exposed skin), and indoor ozone concentration on the total OH reactivity of gaseous human emissions. The results show that the measured concentrations of VOCs and ammonia adequately account for the measured total OH reactivity. The total OH reactivity of human emissions was primarily affected by ozone reactions with organic skin-oil constituents and increased with exposed skin surface, higher temperature, and higher humidity. Humans emitted a comparable total mixing ratio of VOCs and ammonia at elevated temperature-low humidity and elevated temperature-high humidity, with relatively low diversity in chemical classes. In contrast, the total OH reactivity increased with higher temperature and higher humidity, with a larger diversity in chemical classes compared to the total mixing ratio. Ozone present, carbonyl compounds were the dominant reactive compounds in all of the reported conditions.