A. Souza, M. Abreu, J. F. Oliveira‐Júnior, F. Aristone, W. A. Fernandes, R. Graf, Taynã Maria Pinto Lins, Carlos José Reis
{"title":"巴西中西部夜间地面臭氧浓度:NO和NO2浓度分配","authors":"A. Souza, M. Abreu, J. F. Oliveira‐Júnior, F. Aristone, W. A. Fernandes, R. Graf, Taynã Maria Pinto Lins, Carlos José Reis","doi":"10.17628/ECB.2021.10.191-198","DOIUrl":null,"url":null,"abstract":"The contribution of the precursors nitric oxide (NO), nitrogen dioxide (NO 2 ), and meteorological factors were evaluated in relation to the formation of nocturnal O 3 in Campo Grande – MS, Brazil. The maximum nocturnal level identified in the study for NO 2 , NO, and O 3 were 49.5, 58.0, and 30.0 μg.m -3 ,followed by the minimum values of 10.0, 6.0, and 9.0 μg m -3 and averages of 27.4, 21.2, and 18.3 μg m -3 , respectfully. The effect of NO 2 and NO titration emitted by anthropic sources in the urban area, which has the highest levels of NO 2 and NO in comparison with other locations, may be the main driving force of the lowest nocturnal O 3 value. During the night, O 3 titration at ground level occurred, resulting in the average value of the ratio, recorded as 25.6 with maximum and minimum values of 35.4 and 19.8 μg m -3 . It suggests that urban locations with wind speeds values of positive can lead to the accumulation of O 3 at night. The average ratio between the concentration of nocturnal ozone and diurnal surface ozone for Campo Grande was 55%.","PeriodicalId":11880,"journal":{"name":"European Chemical Bulletin","volume":"10 1","pages":"191-198"},"PeriodicalIF":0.0000,"publicationDate":"2021-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"NIGHTLY OZONE CONCENTRATIONS AT GROUND LEVEL IN THE MIDWEST OF BRAZIL: NO AND NO2 CONCENTRATION ASSIGNMENTS\",\"authors\":\"A. Souza, M. Abreu, J. F. Oliveira‐Júnior, F. Aristone, W. A. Fernandes, R. Graf, Taynã Maria Pinto Lins, Carlos José Reis\",\"doi\":\"10.17628/ECB.2021.10.191-198\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The contribution of the precursors nitric oxide (NO), nitrogen dioxide (NO 2 ), and meteorological factors were evaluated in relation to the formation of nocturnal O 3 in Campo Grande – MS, Brazil. The maximum nocturnal level identified in the study for NO 2 , NO, and O 3 were 49.5, 58.0, and 30.0 μg.m -3 ,followed by the minimum values of 10.0, 6.0, and 9.0 μg m -3 and averages of 27.4, 21.2, and 18.3 μg m -3 , respectfully. The effect of NO 2 and NO titration emitted by anthropic sources in the urban area, which has the highest levels of NO 2 and NO in comparison with other locations, may be the main driving force of the lowest nocturnal O 3 value. During the night, O 3 titration at ground level occurred, resulting in the average value of the ratio, recorded as 25.6 with maximum and minimum values of 35.4 and 19.8 μg m -3 . It suggests that urban locations with wind speeds values of positive can lead to the accumulation of O 3 at night. The average ratio between the concentration of nocturnal ozone and diurnal surface ozone for Campo Grande was 55%.\",\"PeriodicalId\":11880,\"journal\":{\"name\":\"European Chemical Bulletin\",\"volume\":\"10 1\",\"pages\":\"191-198\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-01-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"European Chemical Bulletin\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.17628/ECB.2021.10.191-198\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"Chemistry\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"European Chemical Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.17628/ECB.2021.10.191-198","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Chemistry","Score":null,"Total":0}
NIGHTLY OZONE CONCENTRATIONS AT GROUND LEVEL IN THE MIDWEST OF BRAZIL: NO AND NO2 CONCENTRATION ASSIGNMENTS
The contribution of the precursors nitric oxide (NO), nitrogen dioxide (NO 2 ), and meteorological factors were evaluated in relation to the formation of nocturnal O 3 in Campo Grande – MS, Brazil. The maximum nocturnal level identified in the study for NO 2 , NO, and O 3 were 49.5, 58.0, and 30.0 μg.m -3 ,followed by the minimum values of 10.0, 6.0, and 9.0 μg m -3 and averages of 27.4, 21.2, and 18.3 μg m -3 , respectfully. The effect of NO 2 and NO titration emitted by anthropic sources in the urban area, which has the highest levels of NO 2 and NO in comparison with other locations, may be the main driving force of the lowest nocturnal O 3 value. During the night, O 3 titration at ground level occurred, resulting in the average value of the ratio, recorded as 25.6 with maximum and minimum values of 35.4 and 19.8 μg m -3 . It suggests that urban locations with wind speeds values of positive can lead to the accumulation of O 3 at night. The average ratio between the concentration of nocturnal ozone and diurnal surface ozone for Campo Grande was 55%.