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Titlebook: Atmospheric Microbial Aerosols; Theory and Applicati Bruce Lighthart,Alan Jeff Mohr Book 1994 Chapman & Hall, Inc. 1994 ecosystem.environme

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https://doi.org/10.1007/978-3-531-19185-0rvival of organisms contained in the droplets. Combined effects of the dispersion, removal, and survival of microorganisms in sprayed droplets determine the area and period affected by sprayed aerosols.
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Die Quadrattafel und die Wurzeltafel,d picture of all types of bioaerosol-surface interactions. To approximate the situation, it is necessary to introduce several simplifying assumptions, which are guided by knowledge of less complex aerosol systems.
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Reinhard Pöschel,Lev A. Kalužninons are far removed from conditions in the “natural” environment. In the latter case, the microorganisms are subjected to consistent fluxes in very low (“suboptimal”) levels of nutrients. Attempts to grow these microorganisms in a laboratory environment where nutrients are plentiful often stresses microorganisms and impairs their ability to grow.
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Introduction,ion (or condensation), leaving an aeroplanktonic residue of nonvolatile solute, particulate matter and/or viable or non-viable microoganisms. (To avoid the confusion of the changing condition of a liquid droplet evaporating to a dry particle, bioaerosols in this state will be termed droplet/particles or D/Ps.)
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Book 1994micalto the meteorological andmicrobial. It will be of great interest asa starting point forresearchers interested in outdoor microbialbioaerosols as well asfor those interested in atmospheric dispersionmodels, new equipment,and government regulations.
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Death Mechanisms in Microbial Bioaerosols with Special Reference to the Freeze-Dried Analog,owders of microorganisms in his biotechnological applications in manufacturing, agriculture, and forestry. Although, airborne, the deleterious effects of the stressful atmospheric conditions may damage the organisms, there is a point where resuscitation repair is necessary,. or a point beyond repair (i.e., death).
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Dispersion Models of Microbial Bioaerosols,flux (i.e., D/P transfer rate where D/P is a droplet/particle; D/P/M. s.) of bioaerosols from a source that contributes to the loading of the bulk atmosphere (Fig. 9.1) through comprehensive, theoretical, and multiple regression models characterizing the factors that affect the survival of airborne microbes (Larson, 1973) [Eq. (9.1)].
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