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Nighttime formation of peroxy and hydroxyl radicals during the BERLIOZ campaign: Observations and modeling studies
119
Citations
49
References
2003
Year
Radical EmissionEngineeringNitrate RadicalAtmospheric PhotochemistryOrganic ChemistryChemistryEnvironmental PhotochemistryNocturnal Radical ChemistryEarth ScienceOxidative StressEnvironmental ChemistryAtmospheric ScienceOzone Layer DepletionHealth SciencesNighttime FormationPhotochemistryRadical (Chemistry)OzoneHydroxyl RadicalsRo 2SpectroscopyBerlioz Campaign
Traditionally, tropospheric radical chemistry is discussed in terms of the daytime photochemically produced hydroxyl radical (OH). Radicals, however, are also important during nighttime: this is especially true for ozone and the nitrate radical (NO 3 ), which both act as key initiators of the degradation of alkenes such as biogenic monoterpenes. These reactions lead to the formation of peroxy radicals (HO 2 and RO 2 ) and hydroxyl radicals at night. We present recent observations of nighttime concentrations of NO 3 , RO 2 , HO 2 , and OH by differential optical absorption spectroscopy (DOAS), matrix isolation electron spin resonance (MIESR), laser‐induced fluorescence (LIF), and a chemical amplifier (CA) in the framework of the Berliner Ozonexperiment (BERLIOZ) campaign at Pabstthum, Germany, together with modeling studies of nocturnal radical chemistry. Modeled RO 2 mixing ratios reached 40 ppt while the measured RO x level went up to 22 ppt at the same time. Modeled and measured HO 2 mixing ratios were up to 6 and 4 ppt, respectively. In the case of OH, a nocturnal concentration of (1.85 ± 0.82) × 10 5 cm −3 was measured during one night. At this time, the model yielded an OH level of (4.1 ± 0.7) × 10 5 cm −3 . This overestimation by the model could point to a missing nocturnal sink of OH. Nitrate radical reactions with terpenes were found responsible for producing 77% of the RO 2 radicals, 53% of the HO 2 , and 36% of the OH radicals during night. Nighttime ozonolysis formed 12% of the RO 2 , 47% of the HO 2 , and 64% of the OH radicals. Another 11% of the RO 2 radicals were formed by OH–volatile organic compound (VOC) reactions. A positive linear correlation of RO 2 and NO 3 was observed and could be reproduced in model calculations originating from the loss of both radicals by reaction with NO and the NO 3 ‐initiated RO 2 production. The contribution of nighttime OH to the atmosphere's oxidation capacity (oxidation rate of VOCs, CO, and CH 4 ) was found negligible (<0.5%).
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