Abstract

Abstract. Primary Biological Aerosol Particles (PBAPs), including bacteria, spores and pollen, are essential for the spread of organisms and disease in the biosphere, and numerous studies have suggested that they may be important for atmospheric processes, including the formation of clouds and precipitation. The atmospheric abundance and size distribution of PBAPs, however, are largely unknown. At a semi-urban site in Mainz, Germany we used an Ultraviolet Aerodynamic Particle Sizer (UV-APS) to measure Fluorescent Biological Aerosol Particles (FBAPs), which provide an estimate of viable bioaerosol particles and can be regarded as an approximate lower limit for the actual abundance of PBAPs. Fluorescence of non-biological aerosol components are likely to influence the measurement results obtained for fine particles (<1 μm), but not for coarse particles (1–20 μm). Averaged over the four-month measurement period (August–December 2006), the mean number concentration of coarse FBAPs was ~3×10−2 cm−3, corresponding to ~4% of total coarse particle number. The mean mass concentration of FBAPs was ~1μg m−3, corresponding to ~20% of total coarse particle mass. The FBAP number size distributions exhibited alternating patterns with peaks at various diameters. A pronounced peak at ~3 μm was essentially always observed and can be described by the following campaign-average lognormal fit parameters: geometric mean diameter 3.2 μm, geometric standard deviation 1.3, number concentration 1.6×10−2 cm−3. This peak is likely due to fungal spores or agglomerated bacteria, and it exhibited a pronounced diel cycle (24-h) with maximum intensity during early/mid-morning. FBAP peaks around ~1.5 μm, ~5 μm, and ~13 μm were also observed, but less pronounced and less frequent. These may be single bacterial cells, larger fungal spores, and pollen grains, respectively. The observed number concentrations and characteristic sizes of FBAPs are consistent with microscopic, biological and chemical analyses of PBAPs in aerosol filter samples. To our knowledge, however, this is the first exploratory study reporting continuous online measurements of bioaerosol particles over several months and a range of characteristic size distribution patterns with a persistent bioaerosol peak at ~3 μm. The measurement results confirm that PBAPs account for a substantial proportion of coarse aerosol particle number and mass in continental boundary layer air. Moreover, they suggest that the number concentration of viable bioparticles is dominated by fungal spores or agglomerated bacteria with aerodynamic diameters around 3 μm rather than single bacterial cells with diameters around 1 μm.

Highlights

  • Biogenic aerosols are ubiquitous in the Earth’s atmosphere and they play important roles in atmospheric chemical and physical processes, climate, biological systems, and public health (Cox and Wathes, 1995; Poschl, 2005; Jaenicke et al, 2007)

  • Available information suggests that coarse fluorescent particles (>1 μm) measured by the Ultraviolet Aerodynamic Particle Sizer (UV-APS) can be regarded as “Fluorescent Biological Aerosol Particles” (FBAP), which provide an estimate of viable bioaerosol particles and whose abundance represents an approximate lower limit for the actual abundance of primary biological aerosol particles

  • The results show that FBAPs account for a small but significant fraction of total coarse aerosol particle number in the investigated size range (1–20 μm), and they indicate that the sources and sinks of FBAPs are less variable than those of other types of aerosol particles in Central Europe

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Summary

Introduction

Biogenic aerosols are ubiquitous in the Earth’s atmosphere and they play important roles in atmospheric chemical and physical processes, climate, biological systems, and public health (Cox and Wathes, 1995; Poschl, 2005; Jaenicke et al, 2007). Huffman et al.: Fluorescent biological aerosol particle concentrations and size distributions and characteristic size ranges of PBAP are viruses (0.01– 0.3 μm), bacteria (0.1–10 μm), fungal and fern spores (1– 30 μm), plant pollen (5–100 μm), and fragments of animal and plant matter Many organisms rely on bioaerosols for the distribution and transfer of genetic material for reproductive purposes, as in the cases of plant pollen and fungal spores, which can undergo transport over long distances (Elbert et al, 2007, and referencse therein). PBAPs may influence climate and the hydrological cycle by initiating the formation of clouds and precipitation as cloud condensation and ice nuclei (Dingle, 1966; Schnell and Vali, 1972; Hamilton and Lenton, 1998; Diehl et al, 2001; Lohmann and Feichter, 2005; Dusek et al, 2006; McFiggans et al, 2006; Sun and Ariya, 2006; Christner et al, 2008; Deguillaume et al, 2008; Morris et al, 2008; Mortazavi et al, 2008; Rosenfeld et al, 2008; Ariya et al, 2009; Bowers et al, 2009; Pratt et al, 2009; Prenni et al, 2009)

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