J. Burkert , T. Behmann , M.D. Andrés Hernández , D. Stöbener , M. Weißenmayer , D. Perner , J.P. Burrows
{"title":"葡萄牙森林地区过氧自由基的测量","authors":"J. Burkert , T. Behmann , M.D. Andrés Hernández , D. Stöbener , M. Weißenmayer , D. Perner , J.P. Burrows","doi":"10.1016/S1465-9972(01)00014-9","DOIUrl":null,"url":null,"abstract":"<div><p>As part of the FIELDVOC'94 study, ambient concentrations of peroxy radicals (RO<sub>2</sub>, R=H, CH<sub>3</sub>, CH<sub>3</sub>CO, etc.) were continuously measured at a forested site in Portugal, using the chemical amplification technique. The amount of RO<sub>2</sub> varied between 0 and 260 pptv with maximum values being obtained under clear sky conditions. The RO<sub>2</sub> mixing ratio correlates with that of isoprene. The rate of production of ozone, O<sub>3</sub>, indicates that the noon-time maximum values lay between 5 and 17 ppbv h<sup>−1</sup>. On several days, the maximum O<sub>3</sub> mixing ratio at this rural site was similar to that found in urban areas, which experience smog episodes (O<sub>3</sub> mixing ratio<!--> <!-->><!--> <!-->90 ppbv). The RO<sub>2</sub> estimated assuming a photostationary state RO<sub>2</sub>,(PSS) of NO<sub>2</sub>, NO and O<sub>3</sub>, was not found to have a significant statistical correlation with the measured RO<sub>2</sub>. The latter is best explained by the errors associated with the calculation of RO<sub>2</sub>,(PSS) at low NO<sub><em>x</em></sub> (NO<!--> <!-->+<!--> <!-->NO<sub>2</sub>) mixing ratios. The diurnal behavior of O<sub>3</sub> in the boundary layer was estimated using a relatively simple source/sink parameterization. On days having high O<sub>3</sub> mixing ratios, both predicted and observed O<sub>3</sub> behavior agree well. For days having O<sub>3</sub> mixing ratios<!--> <!--><<!--> <!-->75 ppbv, it was found that the simple parameterization needed to be extended to include entrainment of O<sub>3</sub> after dawn from above the night-time inversion layer.</p></div>","PeriodicalId":100235,"journal":{"name":"Chemosphere - Global Change Science","volume":"3 3","pages":"Pages 327-338"},"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)00014-9","citationCount":"27","resultStr":"{\"title\":\"Measurements of peroxy radicals in a forested area of Portugal\",\"authors\":\"J. Burkert , T. Behmann , M.D. Andrés Hernández , D. Stöbener , M. Weißenmayer , D. Perner , J.P. Burrows\",\"doi\":\"10.1016/S1465-9972(01)00014-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>As part of the FIELDVOC'94 study, ambient concentrations of peroxy radicals (RO<sub>2</sub>, R=H, CH<sub>3</sub>, CH<sub>3</sub>CO, etc.) were continuously measured at a forested site in Portugal, using the chemical amplification technique. The amount of RO<sub>2</sub> varied between 0 and 260 pptv with maximum values being obtained under clear sky conditions. The RO<sub>2</sub> mixing ratio correlates with that of isoprene. The rate of production of ozone, O<sub>3</sub>, indicates that the noon-time maximum values lay between 5 and 17 ppbv h<sup>−1</sup>. On several days, the maximum O<sub>3</sub> mixing ratio at this rural site was similar to that found in urban areas, which experience smog episodes (O<sub>3</sub> mixing ratio<!--> <!-->><!--> <!-->90 ppbv). The RO<sub>2</sub> estimated assuming a photostationary state RO<sub>2</sub>,(PSS) of NO<sub>2</sub>, NO and O<sub>3</sub>, was not found to have a significant statistical correlation with the measured RO<sub>2</sub>. The latter is best explained by the errors associated with the calculation of RO<sub>2</sub>,(PSS) at low NO<sub><em>x</em></sub> (NO<!--> <!-->+<!--> <!-->NO<sub>2</sub>) mixing ratios. The diurnal behavior of O<sub>3</sub> in the boundary layer was estimated using a relatively simple source/sink parameterization. On days having high O<sub>3</sub> mixing ratios, both predicted and observed O<sub>3</sub> behavior agree well. For days having O<sub>3</sub> mixing ratios<!--> <!--><<!--> <!-->75 ppbv, it was found that the simple parameterization needed to be extended to include entrainment of O<sub>3</sub> after dawn from above the night-time inversion layer.</p></div>\",\"PeriodicalId\":100235,\"journal\":{\"name\":\"Chemosphere - Global Change Science\",\"volume\":\"3 3\",\"pages\":\"Pages 327-338\"},\"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)00014-9\",\"citationCount\":\"27\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemosphere - Global Change Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1465997201000149\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemosphere - Global Change Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1465997201000149","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Measurements of peroxy radicals in a forested area of Portugal
As part of the FIELDVOC'94 study, ambient concentrations of peroxy radicals (RO2, R=H, CH3, CH3CO, etc.) were continuously measured at a forested site in Portugal, using the chemical amplification technique. The amount of RO2 varied between 0 and 260 pptv with maximum values being obtained under clear sky conditions. The RO2 mixing ratio correlates with that of isoprene. The rate of production of ozone, O3, indicates that the noon-time maximum values lay between 5 and 17 ppbv h−1. On several days, the maximum O3 mixing ratio at this rural site was similar to that found in urban areas, which experience smog episodes (O3 mixing ratio > 90 ppbv). The RO2 estimated assuming a photostationary state RO2,(PSS) of NO2, NO and O3, was not found to have a significant statistical correlation with the measured RO2. The latter is best explained by the errors associated with the calculation of RO2,(PSS) at low NOx (NO + NO2) mixing ratios. The diurnal behavior of O3 in the boundary layer was estimated using a relatively simple source/sink parameterization. On days having high O3 mixing ratios, both predicted and observed O3 behavior agree well. For days having O3 mixing ratios < 75 ppbv, it was found that the simple parameterization needed to be extended to include entrainment of O3 after dawn from above the night-time inversion layer.