Measurements of hydrogen peroxide and individual organic peroxides in the marine troposphere

Concentrations of gas-phase H 2O 2 and organic peroxides were measured in the marine boundary layer, during the FIELDVOC 93-campaign at the Pointe de Penmarc'h (Brittany, France), from 14 May to 10 June, 1993. Air samples were collected by the scrubber sampling method. Precipitation samples wer...

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Veröffentlicht in:Atmospheric environment (1994) 1997-04, Vol.31 (8), p.1173-1184
Hauptverfasser: Sauer, Frank, Limbach, Stefan, Moortgat, Geert K.
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Sprache:eng
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Zusammenfassung:Concentrations of gas-phase H 2O 2 and organic peroxides were measured in the marine boundary layer, during the FIELDVOC 93-campaign at the Pointe de Penmarc'h (Brittany, France), from 14 May to 10 June, 1993. Air samples were collected by the scrubber sampling method. Precipitation samples were taken during different rain events. Analysis was performed with a reversed-phase high-performance liquid chromatography system (HPLC) using the p-hydroxyphenyl ethanoic acid/peroxidase fluorescence reaction for detection. Gaseous H 2O 2 mixing ratios were found to be < 0.1–1.2 ppbv. No significant diurnal variations of H 2O 2 concentrations were observed. The highest levels of H 2O 2 were measured during a period of pure maritime influence (30 May to 3 June), corresponding to local winds from western and southwestern directions. No organic peroxides were observed in the air samples. Rain water samples showed H 2O 2 concentrations of 1.4–134.8 μmol l −1. The highest concentration was measured on 27 May during a heavy thunderstorm. Organic peroxides, HOCH 2OOH (HMHP) and CH 3CH(OH)OOH (1-HEHP), were detected in rain samples with concentrations in the range of 0.4–0.8 μmol l −1. Meteorological parameters and trace gas concentrations, measured by other groups participating in the campaign, were taken into account to study their correlation with atmospheric peroxide concentrations. The results from the correlation analysis showed that the concentration of gaseous H 2O 2 is strongly dependent on the ambient concentration of NO x .
ISSN:1352-2310
1873-2844
DOI:10.1016/S1352-2310(96)00289-0