2003
DOI: 10.1016/s0048-9697(03)00250-x
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Volatile organic compounds in rural atmospheres of central Portugal

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Cited by 55 publications
(23 citation statements)
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“…This observation is consistent with the fact that photochemical activities are generally stronger on days with more hours of sunlight, which are frequently warmer days, leading to higher production of secondary carbonyl compounds in the atmosphere. [31][32][33] Recent studies conducted in urban areas of Rome, Italy, and at a semirural site in Denmark showed similar seasonal variations in ambient carbonyl concentrations for most of the carbonyl compounds measured in this study, with highest concentrations observed during summer times. 27,34 The exception was formaldehyde in the current study.…”
Section: Resultssupporting
confidence: 81%
“…This observation is consistent with the fact that photochemical activities are generally stronger on days with more hours of sunlight, which are frequently warmer days, leading to higher production of secondary carbonyl compounds in the atmosphere. [31][32][33] Recent studies conducted in urban areas of Rome, Italy, and at a semirural site in Denmark showed similar seasonal variations in ambient carbonyl concentrations for most of the carbonyl compounds measured in this study, with highest concentrations observed during summer times. 27,34 The exception was formaldehyde in the current study.…”
Section: Resultssupporting
confidence: 81%
“…A possible explanation for the higher concentrations detected in summer could be transport of pollutants from the coast by sea breezes, that are of regular occurrence during summer days. It has been shown, for example, that during summer the air in central Iberian Peninsula contains recirculated pollutants from previous days or emitted from densely populated along coast [6].…”
Section: Resultsmentioning
confidence: 99%
“…Glyoxal is very water soluble, and it has an air-seawater partition coefficient, K, of 3.6 × 10 5 M atm − 1 at 25°C . Reported glyoxal concentrations in the atmosphere are 0.025-0.14 ppbv over the remote tropical Pacific Ocean (Sinreich et al, 2010), 0.05-0.6 ppbv in a rural area in Portugal (Cerqueira et al, 2003), 0.13 ppbv in a city in China (Dai et al, 2012), and 0.07 ppbv in a suburban area in Japan (Ortiz et al, 2006(Ortiz et al, , 2009. Atmospheric glyoxal is primarily produced by oxidation of biogenic and anthropogenic volatile organic compounds (Volkamer et al, 2001;Vrekoussis et al, 2009;Sinreich et al, 2010).…”
Section: Tablementioning
confidence: 99%