Blooming trees as a source of fine (< 5&#956;m) aerosol particles
Authors: Gratzl Jürgen , Seifried Teresa M , Bieber Paul , Grothe Hinrich , Burkart Julia 
Published: March 2020

&lt;p&gt;During the blooming season of trees, pollen is an important component of the atmospheric aerosol, even in urban areas. Wind pollinated plants such as early flowering trees (e.g. birch, alder) release pollen grains in extremely large quantities. Once in the atmosphere pollen can impact human health and cloud formation (Sch&amp;#228;ppi et al. 1999, Pummer et al. 2012, Steiner et al. 2015). Intact pollen grains are rather large with geometrical diameters from 10-100 &amp;#956;m and therefore have short residence times in the atmosphere. However, it is known that under certain conditions (high humidity and after germination) pollen grains release cytoplasmic material including starch granules from their interior, commonly referred to as subpollen particles (SPP). Studies have shown that the cytoplasmic material contains cloud active substances and allergens (Steiner et al. 2015, Pummer et al. 2012, Basci et al. 2006). How and if this material becomes airborne and whether it distributes in the atmosphere is still an open question. Motivated by this question we took a detailed look at the particles shed from blooming catkins.&lt;/p&gt;
&lt;p&gt;In this study freshly harvested branches with flowering catkins of different trees were put in an aerosol chamber. An Aerodynamic Particle Sizer (TSI Spectrometer 3321; 0.5 &amp;#8211; 20 &amp;#956;m) and a Cascade Impactor (Sioutas; 2.5 &amp;#956;m, 1.0 &amp;#956;m, 0.50 &amp;#956;m, 0.25 &amp;#956;m) were attached to the chamber to sample the released aerosol. The catkins were agitated with puffs of clean air to simulate wind. The aerodynamic diameters of the released particles were recorded and the filters of the impactor were analyzed with a Scanning Electron Microscope and a light microscope. We find that not only large pollen grains are released but also smaller particles. Up to 50% of all released particles were in the size range from (0.5 &amp;#8211; 5 &amp;#956;m). Additionally, we find that the aerodynamic diameter of pollen grains is in general smaller than their geometrical diameter. For instance, the aerodynamic diameter of pollen grains from birch is 30-70% smaller than the geometrical diameter.&lt;/p&gt;
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&lt;p&gt;References:&lt;br /&gt;Sch&amp;#228;ppi, G. F.; Taylor, P. E.; Pain, M. C.; Cameron, P. A.; Dent, A. W.; Staff, I. A. &amp; Suphioglu, C.; Concentrations of major grass group 5 allergens in pollen grains and atmospheric particles: implications for hay fever and allergic asthma sufferers sensitized to grass pollen allergens.; Clinical and experimental allergy: journal of the British Society for Allergy and Clinical Immunology, 1999, 29, 633-641&lt;br /&gt;Pummer, B. G.; Bauer, H.; Bernardi, J.; Bleicher, S. &amp; Grothe, H.; Suspendable macromolecules are responsible for ice nucleation activity of birch and conifer pollen; Atmospheric Chemistry and Physics, Copernicus GmbH, 2012, 12, 2541-2550&lt;br /&gt;Steiner, A. L.; Brooks, S. D.; Deng, C.; Thornton, D. C. O.; Pendleton, M. W. &amp; Bryant, V.; Pollen as atmospheric cloud condensation nuclei; Geophysical research letters, Wiley Online Library, 2015, 42, 3596-3602&lt;br /&gt;Bacsi, A.; Choudhury, B. K.; Dharajiya, N.; Sur, S. &amp; Boldogh, I.; Subpollen particles: carriers of allergenic proteins and oxidases; Journal of Allergy and Clinical Immunology, Elsevier, 2006 , 118 , 844-850&lt;/p&gt;