Chapter 5 Aeromicrobiology Ian L. Pepper and Scot E. Dowd 1. List

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Chapter 5

Aeromicrobiology

Ian L. Pepper and Scot E. Dowd

List some beneficial microorganisms not described in the text that are spread via the aeromicrobiological pathway.

Soil particulate material that routinely becomes aerosolized during high wind conditions also contains large populations of aerosolized bacteria which are heterotrophic plate count (HPCs). The majority of

HPCs aerosolized are non-pathogenic and mimic the normal soil microflora. Therefore, aerosolized HPCs are a mechanism for dispersing microbes spatially and enhancing diversity. As an example this provides a mechanism for dispersion of biodegradative genes or nitrogen fixing bacteria. In theory any beneficial microbe found in soil can become aerosolized.

Describe the AMB pathway for hantavirus including launching mechanisms, transportation mechanisms, and deposition mechanisms.

Hantavirus:

Launching: wind

Transportation: wind

Deposition: gravitational settling; rain deposition

Give an example of a continuous linear source and an example of an instantaneous area source of bioaerosols.

Continuous linear sources of bioaerosol = biosolid applicator moving across a field

Instantaneous area source of bioaerosol = endotoxin associated with soil particulates during a wind gust across a field.

Considering a wind speed of 1.5 m/s, an object that is 12 cm tall, and normal air viscosity, determine whether conditions around the object would be considered turbulent.

Conditions around the object would not be considered turbulent due to a low Reynolds Number

Consider an airborne virus and airborne protozoan with a radius of 30 mm and 1 μm and particle densities of 2.0 and 1.1 g/cm 3 , respectively. Under normal gravitational acceleration calculate the terminal velocity for each.

Use Stokes Law:

V

D

2 x (

 p

 

1

18

) x g

Where v = velocity of fall

6. g = acceleration of gravity (980 cm sec

-2 )

D = diameter of particle (cm)

ρ p

= density of particle g/cm 3 = 2.0 for virus and 1.1 for protozoa

ρ

1

= density of air

ζ = viscosity of air

Due to smaller size of virus, virus descends much more slowly than protozoa.

Calculate the annual community risk of infection given the following data: aerosolized virus concentration = 7.16/cm 3 of air, duration of exposure = 8h, infectivity constant r = 0.0253, and breathing rate = 0.83 m 3 /h.

Probability of infection [per day = ρ i

= 1 - exp (-4N)

Where r = infectivity constant = 0.0253

N = number of pathogens inhaled per day

Here N

.

69

∴ ρ i = 1 - exp (-0.0253 x 69)

Annual risk = P year

= 1 - (1 - ρ i

) d

Where d = 2 days

∴ P year

= 1 - (1 - ρ i

) 2

P year

= 0.96

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