Artigo Revisado por pares

Organic acids and aldehydes in rainwater in a northwest region of Spain

2002; Elsevier BV; Volume: 36; Issue: 34 Linguagem: Inglês

10.1016/s1352-2310(02)00648-9

ISSN

1873-2844

Autores

Rosa M Peña, S. Garcı́a Martı́n, Carlos Herrero, M. Losada, Ana Vázquez, T. Lucas,

Tópico(s)

Air Quality Monitoring and Forecasting

Resumo

During a 1 year period, measurements of carboxylic acids and aldehydes were carried out in rainwater samples collected at nine different sites in NW Spain surrounding a thermal power plant in order to determine concentration levels and sources. In addition, certain major ions (Cl−, NO3−, SO42−, Na+, NH4+, K+, Mg2+, Ca2+) were also determined. Aldehyde and carboxylic acid concentration patterns and their effects on rainwater composition concerning temporal, seasonal and spatial variations were evaluated. Among carboxylic acids, formic and acetic were predominant (VWA 7.0 and 8.3 μM), while formaldehyde and acroleine were the dominant aldehydes (VWA 0.42 and 1.25 μM). Carboxylic acids were estimated to account for 27.5% of the total free acidity (TFA), whereas sulphuric and nitric acid accounted for 46.2% and 26.2%, respectively. Oxalic acid was demonstrated to be an important contributing compound to the acidification in rainwater representing 7.1% of the TFA. The concentration of aldehydes and carboxylic acids, which originated mainly from biogenic emissions in the area studied, was strongly dependent on the season of the year (growing and non-growing). The ratios of formic to acetic acids are considerably different in the two seasons suggesting that there exist distinct sources in both growing and non-growing seasons. Principal component analysis was applied in order to elucidate the sources of aldehydes and organic acids in rainwater. The prevalence of natural vegetative origins for both of these compounds versus anthropogenic emissions was demonstrated and the importance of the oxidation of aldehydes as a relevant source of organic acids was also established.

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