Abstract
This study provides the first data set of (210)Po and (210)Pb activity concentrations in the organic and inorganic components of several particle size classes of aerosols collected at two sampling stations in Kuwait. The (210)Po concentrations in the aerosols (Bq/g) were similar in all of the particle size classes, but as most (91%) of the aerosol load was made of fine fraction particles of PM(0.39-2.5) (µm), most of the (210)Po activity was carried by this aerosol fraction. At the two sampling stations, the (210)Po/(210)Pb activity concentration ratios in the aerosols were similar, stable around the year, and averaged 1.5 (range 1.2-1.9), much higher than the typical activity concentration ratios of these radionuclides in unmodified (background) aerosols, with Po/Pb < 0.1. The aerosol enrichment in (210)Po was likely originated from the oil industry, specifically by gas flaring and oil refining in the Gulf region. Radionuclide analysis in the organic and inorganic components of aerosols showed that the (210)Po concentration in the organic component was one order of magnitude higher than the (210)Po concentration in the inorganic component, in contrast with (210)Pb, which displayed similar concentrations in both organic and inorganic aerosol components. The (210)Po carrying organic component of aerosols was investigated and it was found to be largely composed of microorganisms with high microbial and fungi diversity, with the phyla Proteobacteria, Ascomycota, and Basidiomycota being dominant among the bacteria and with Zygomycota being dominant among the fungi. Therefore, we are facing an active concentration process of the atmospheric (210)Po carried out by microorganisms, which underlies the (210)Po enrichment process in the organic component of aerosols. This bioconcentration of polonium in bioaerosols was unknown.