Applied and Environmental Microbiology · 1982 · 275 citations · 31 references
AgricultureAgronomyCrop SciencesMicrobial EcologyPlant-microbe InteractionsSoil MicrobiologyBacterial EcologyBacterial SurvivalRhizosphere MicrobiologySoil Microbial PhysiologyAirborne Bacterial DiversityBare Soil FractionColony-forming Unit EnumerationConcentrationConcentration GradientsIce Nucleation Active BacteriaIce Nucleation ProcessesViable Cell Count
Vertical wind shear and concentration gradients of viable, airborne bacteria were used to calculate the upward flux of viable cells above bare soil and canopies of several crops. Concentrations at soil or canopy height varied from 46 colony-forming units per m over young corn and wet soil to 663 colony-forming units per m over dry soil and 6,500 colony-forming units per m over a closed wheat canopy. In simultaneous samples, concentrations of viable bacteria in the air 10 m inside an alfalfa field were fourfold higher than those over a field with dry, bare soil immediately upwind. The upward flux of viable bacteria over alfalfa was three- to fourfold greater than over dry soil. Concentrations of ice nucleation-active bacteria were higher over plants than over soil. Thus, plant canopies may constitute a major source of bacteria, including ice nucleation-active bacteria, in the air.
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Bergey's Manual of Determinative Bacteriology
F. A. S., R. E. Buchanan, N. E. Gibbons et al. · Taxon · 1975 · 11.4K citations
Two simple media for the demonstration of pyocyanin and fluorescin.
The Microbiology of the Atmosphere
C. L. Kramer, P. H. Gregory · Mycologia · 1974 · 984 citations
Life Sciences, Biology, Microbiology +13