Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9580
AuthorsGranieri, D.* 
Costa, A.* 
Macedonio, G.* 
Bisson, M.* 
Chiodini, G.* 
TitleCarbon dioxide in the urban area of Naples: Contribution and effects of the volcanic source
Issue Date15-Jun-2013
Series/Report no./260 (2013)
DOI10.1016/j.jvolgeores.2013.05.003
URIhttp://hdl.handle.net/2122/9580
KeywordsCO2 dispersion; Solfatara; Gas hazard; Campi Flegrei
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.01. Gases 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
AbstractNaples is a large city located between two active volcanic areas: Campi Flegrei to theWand Vesuvius to the SE. The Solfatara crater, inside the caldera of the Campi Flegrei and nearest to the western quarters of the city, is a prodigious source of natural CO2 with a mean emission rate of 1067 ton/d, i.e. seven times higher than that of Vesuvius(151 ton/d). This study shows that the area around the Solfatara and part of the urban area of Naples are affected by the volcanic plume when atmospheric circulatory patterns are dominated by the locally frequent sea breezes. Under these conditions the CO2 content in the air increases above normal values, reaching more than 1000 ppm in proximity to the Solfatara crater to a few tens of ppm several kilometres from the source. Although these values do not indicate a health risk even under the most unfavourable atmospheric conditions, the volcanic source contributes to the total CO2 burden from all urban emissions and hence to overall air quality. An emission rate ten times higher than the present one would lead to an air CO2 concentration in excess of recommended health protection thresholds.
Appears in Collections:Papers Published / Papers in press

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