A new optical-based technique for real-time measurements of mineral dust concentration in PM.sub.10 using a virtual impactor

• Published in: Atmospheric measurement techniques 2020-07, Vol.13 (7), p.3799
• Main Authors: Drinovec, Luka, Sciare, Jean, Stavroulas, Iasonas, Bezantakos, Spiros, Pikridas, Michael, Unga, Florin, Savvides, Chrysanthos, ViÅ¡ic, Bojana, RemÅ¡kar, Maja, Mocnik, GriÅ¡a
• Format: Article
• Language: English
• ISSN: 1867-1381; 1867-8548

Atmospheric mineral dust influences Earth's radiative budget, cloud formation, and lifetime; has adverse health effects; and affects air quality through the increase of regulatory PM.sub.10 concentrations, making its real-time quantification in the atmosphere of strategic importance. Only few near-real-time techniques can discriminate dust aerosol in PM.sub.10 samples and they are based on the dust chemical composition. The online determination of mineral dust using aerosol absorption photometers offers an interesting and competitive alternative but remains a difficult task to achieve. This is particularly challenging when dust is mixed with black carbon, which features a much higher mass absorption cross section. We build on previous work using filter photometers and present here for the first time a highly time-resolved online technique for quantification of mineral dust concentration by coupling a high-flow virtual impactor (VI) sampler that concentrates coarse particles with an aerosol absorption photometer (Aethalometer, model AE33). The absorption of concentrated dust particles is obtained by subtracting the absorption of the submicron (PM.sub.1) aerosol fraction from the absorption of the virtual impactor sample (VI-PM1 method). This real-time method for detecting desert dust was tested in the field for a period of 2 months (April and May 2016) at a regional background site of Cyprus, in the Eastern Mediterranean. Several intense desert mineral dust events were observed during the field campaign with dust concentration in PM.sub.10 up to 45 µg m.sup.-3 . Mineral dust was present most of the time during the campaign with an average PM.sub.10 of about 8 µg m.sup.-3 . Mineral dust absorption was most prominent at short wavelengths, yielding an average mass absorption cross section (MAC) of 0.24±0.01 m.sup.2  g.sup.-1 at 370 nm and an absorption Ãngström exponent of 1.41±0.29. This MAC value can be used as a site-specific parameter for online determination of mineral dust concentration. The uncertainty of the proposed method is discussed by comparing and validating it with different methods.