{"title":"Hydrogen peroxide, organic peroxides and organic acids in a forested area during FIELDVOC'94","authors":"F. Sauer , J. Beck , G. Schuster , G.K. Moortgat","doi":"10.1016/S1465-9972(01)00013-7","DOIUrl":null,"url":null,"abstract":"<div><p>Gas-phase H<sub>2</sub>O<sub>2</sub>, organic peroxides and organic acids were measured from mid-June to mid-July 1994 during the second FIELDVOC'94 campaign in a forested area near Tábua (Portugal). The site was located in a plantation of eucalyptus trees. Methylhydroperoxide (MHP, CH<sub>3</sub>OOH) and H<sub>2</sub>O<sub>2</sub> were quantified in the air samples. Hydroxymethylhydroperoxide (HMHP, HOCH<sub>2</sub>OOH) was observed occasionally. Formic and acetic acids were the organic acids determined in the ambient air. The hydroperoxides and the organic acids showed pronounced diurnal variations with peak mixing ratios in the early afternoon (12:00–16:00 UT). Sometimes a second maximum was observed in the late afternoon (16:00–20:00 UT). In comparison with the peroxides the maximum organic acid mixing ratios were shifted by 1–2 h. The maximum mixing ratios were 1.38 ppbv (H<sub>2</sub>O<sub>2</sub><span>), 0.64 ppbv (MHP), 0.22 ppbv (HMHP), 2.8 ppbv (formic acid), and 1.5 ppbv (acetic acid). The ratio of formic acid over acetic acid mixing ratios was 1.5. The H</span><sub>2</sub>O<sub>2</sub> mixing ratio was strongly dependent on O<sub>3</sub>,NO<sub><em>x</em></sub>, isoprene, RO<sub><em>x</em></sub> and relative humidity. Mixing ratios of all peroxides were below detection limit (d.l.) (<15 pptv) during night-time. Deposition processes were found to determine the mixing ratios of the hydroperoxides and organic acids during the nights.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"3 3","pages":"Pages 309-326"},"PeriodicalIF":0.0000,"publicationDate":"2001-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1465-9972(01)00013-7","citationCount":"34","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemosphere - Global Change Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1465997201000137","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 34
Abstract
Gas-phase H2O2, organic peroxides and organic acids were measured from mid-June to mid-July 1994 during the second FIELDVOC'94 campaign in a forested area near Tábua (Portugal). The site was located in a plantation of eucalyptus trees. Methylhydroperoxide (MHP, CH3OOH) and H2O2 were quantified in the air samples. Hydroxymethylhydroperoxide (HMHP, HOCH2OOH) was observed occasionally. Formic and acetic acids were the organic acids determined in the ambient air. The hydroperoxides and the organic acids showed pronounced diurnal variations with peak mixing ratios in the early afternoon (12:00–16:00 UT). Sometimes a second maximum was observed in the late afternoon (16:00–20:00 UT). In comparison with the peroxides the maximum organic acid mixing ratios were shifted by 1–2 h. The maximum mixing ratios were 1.38 ppbv (H2O2), 0.64 ppbv (MHP), 0.22 ppbv (HMHP), 2.8 ppbv (formic acid), and 1.5 ppbv (acetic acid). The ratio of formic acid over acetic acid mixing ratios was 1.5. The H2O2 mixing ratio was strongly dependent on O3,NOx, isoprene, ROx and relative humidity. Mixing ratios of all peroxides were below detection limit (d.l.) (<15 pptv) during night-time. Deposition processes were found to determine the mixing ratios of the hydroperoxides and organic acids during the nights.