001     911028
005     20240712101042.0
020 _ _ |a 978-3-95806-653-3
024 7 _ |2 Handle
|a 2128/32740
024 7 _ |2 URN
|a urn:nbn:de:0001-2022112370
037 _ _ |a FZJ-2022-04354
100 1 _ |0 P:(DE-Juel1)176215
|a Hantschke, Luisa
|b 0
|e Corresponding author
|u fzj
245 _ _ |a Oxidation of monoterpenes studied in atmospheric simulation chambers
|f - 2022-11-23
260 _ _ |a Jülich
|b Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag
|c 2022
300 _ _ |a 188
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|s 1669190194_22943
336 7 _ |2 DRIVER
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490 0 _ |a Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment
|v 589
502 _ _ |a Dissertation, Univ. Köln, 2022
|b Dissertation
|c Univ. Köln
|d 2022
520 _ _ |a Monoterpenes are volatile organic compounds (VOC) that are emitted into the atmosphere from biogenic sources, such as trees and vegetation, or from anthropogenic sources, such as consumer care products. The mean global emission of monoterpenes is estimated to be 160 Tg a year. In the atmosphere, the monoterpenes react with the main oxidants, the OH radical, ozone (O3), or nitrate radicals (NO3). Products of these oxidation reactions influence the atmospheric composition. Especially formation and growth of organic aerosols and the formation of ozone canhave effects on air quality, human health and climate warming. The oxidation of atmospheric organic compounds by the OH radical initiates a radical chain reaction that involves hydroperoxy radicals (HO2) and organic peroxy radicals (RO2, R=organic group). Depending on the environment, the RO2 radicals can either undergo bimolecular reactions with NO, HO2 or other RO2, or unimolecular reactions. Unimolecular reactions of RO2 include H-shift reactions and endocyclizations. From these autoxidation reactions, higher oxidized species can be formed rapidly.Whether unimolecular reactions of RO2 are competitive with bimolecular reactions is also highly dependent on the molecules structure. Detailed knowledge about the oxidation mechanism of atmospherically relevant species is crucial for understanding the atmospheres’ oxidation capability
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