aerobiology
DESCRIPTION
Aerobiology. Aerobiology. The interdisciplinary science that deals with the movement and dispersal of bioaerosols The movement of bioaerosols is generally passive and is greatly influenced by the environment The survival of viable bioaerosols is also dependent on the environmental conditions. - PowerPoint PPT PresentationTRANSCRIPT
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Aerobiology
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Aerobiology
• The interdisciplinary science that deals with the movement and dispersal of bioaerosols
• The movement of bioaerosols is generally passive and is greatly influenced by the environment
• The survival of viable bioaerosols is also dependent on the environmental conditions
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Bioaerosols
• Biological agents carried in the air as large molecules, volatile compounds, single particles, or clusters of particles that are living or were released from a living organism
• Particles sizes – typically 0.5m to 100 m
• Capable of eliciting diseases that may be infectious, allergic, or toxigenic with the conditions being acute or chronic
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Aerosols and Respiratory Deposition
• Aerosols 5 microns in diameter are removed in the upper respiratory tract, especially the nose. – Particles are brought to the pharynx by mucociliary
activity of the upper respiratory epithelial mucosa, where they are expectorated or swallowed.
• Swallowed particles containing enteric microbes can initiate enteric infections.
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Aerosols and Respiratory Deposition
• Particles <5 microns in diameter, esp. 1‑3 microns diameter, penetrate to the lower respiratory tract– Can be deposited in the bronchioles, alveolar ducts and alveoli. – Deposition efficiency in lower respiratory tract is ~50% for
particles 1‑2 microns diameter. – Particles <0.5 microns dia. can also be deposited in the lower
respiratory tract, especially particles <0.25 microns dia.– Particles deposited in the lower respiratory tract can be
phagocytized by respiratory (alveolar) macrophages• can be destroyed or • carried to the ciliary escalator, where they are transported
upward to the pharynx.
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Hydroscopicity and Aerosol Deposition in the Respiratory Tract
When inhaled, aerosol particles derived from aqueous fluids pick up moisture (water) while traveling in the respiratory passageways, thereby increasing in size.– Increased size changes deposition site
H2O H2O H2O
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Respiratory Deposition - Impaction• Each time airflow changes due to a bifurcation in the airways,
suspended particles tend to travel along their original path due to inertia and may impact on an airway surface.
• This mechanism is highly dependent on aerodynamic diameter, since the stopping distance for very small particles is quite low.
• Occurs mostly for larger particles that are very close to airway walls, near the first airway bifurcations.
• Therefore, deposition by impaction is greatest in the bronchial region.
• Impaction accounts for the majority of particle deposition on
a mass basis.
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Respiratory Deposition - Sedimentation
• Settling out of particles in the smaller airways of the bronchioles and alveoli, where air flow is low and airway dimensions are small.
• Rate of sedimentation is dependent on the terminal settling velocity of the particles
• Sedimentation plays a greater role in the deposition of particles with larger aerodynamic diameters.
• Hygroscopic particles may grow in size as they pass through the warm, humid air passages, thus increasing the probability of deposition by sedimentation.
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Respiratory Deposition - Interception
• Occurs when a particle contacts an airway surface due to its physical size or shape.
• Unlike impaction, particles that are deposited by interception do not deviate from their air streamlines.
• Most likely to occur in small airways or when the air streamline is close to an airway wall.
• Interception is most significant for fibers, which easily contact airway surfaces do to their length. – Furthermore, fibers have small aerodynamic
diameters relative to their size, so they can often reach the smallest airways.
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Respiratory Deposition - Diffusion
• Primary mechanism for particles <0.5 microns in diameter• Governed by geometric rather than aerodynamic size• Net transport of particles from a region of higher to lower
concentration due to Brownian motion. – Brownian motion: random wiggling motion of a particle
due to the constant bombardment of air molecules. • Occurs mostly when particles have just entered the
nasopharynx• Also most likely to occur in the smaller airways of the
pulmonary (alveolar) region, where air flow is low.
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Concentrations in Air
• Concentrations of indoor bacteria range from <100-1500 cfu/m3; avg 0-500– heated dwellings lower
• Avg concentrations of outdoor bacteria 200-1000
• Avg concentrations of indoor Fungi range from 10-500
• Avg concentrations of Outdoor Fungi range from 100-1000
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Microbial IAQ
• Outdoor spores enter readily
• Many fungi can also amplify indoors – anytime moisture is available fungi can grow on many indoor substrates
• Penicillium, Aspergillus, and Cladosporium are most common indoors
• Many can form mycotoxins – Aspergillus spp and Stachybotrys
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Environmental factors that influence indoor fungal contamination
• Outdoor concentration and type
• Type and rate of ventilation
• Activity levels
• Indoor moisture levels
• Modern building materials
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Indoor air sample
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Typical 80/20 recirculation/ventilation consistent with ASHRAE 62-89
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Dry Air Spora
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Diurnal Rhythm of Cladosporium
Hourly Cladosporium Levels Tulsa May 24, 1999
0
5,000
10,000
15,000
20,000
25,000
30,000
12:00AM
2:00AM
4:00AM
6:00AM
8:00AM
10:00AM
12:00PM
2:00 PM 4:00 PM 6:00 PM 8:00 PM 10:00PM
Sp
ore
s/m
3
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Cladosporium spores peak hourly concentration of >120,000 spores/m3 during a spore plume
Cladosporium , 30 September 1998
Tulsa
0
20,000
40,000
60,000
80,000
100,000
120,000
140,000
0:00 2:00 4:00 6:00 8:00 10:00 12:00 14:00 16:00 18:00 20:00 22:00
Spore
s/m3
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Basidiospore Rhythm
• Need for moisture confines spore release to periods of high humidity
• Typically peak levels in pre-dawn hours and low levels in afternoon
May of 1998
0
500
1000
1500
2000
2500
2:00
AM
4:00
AM
6:00
AM
8:00
AM
10:0
0 AM
12:0
0 PM
2:00
PM
4:00
PM
6:00
PM
8:00
PM
10:0
0 PM
12:0
0 AM
spor
es/m
3
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Airborne Fungal Spore Concentrations in Tulsa 2002
0
10,000
20,000
30,000
40,000
50,000
60,000
Sp
ore
s/m
3
0
10,000
20,000
30,000
40,000
50,000
60,000
Sp
ore
s/m
3
2002
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23 Taxa identified: Cladosporium, Ascospores, Basidiospores, and Alternaria Comprised 90% of
Total
Basidiospores
0
500
1000
1500
2000
2500
3000
3500
4000
4500
5000
1/1 2/1 3/1 4/1 5/1 6/1 7/1 8/1 9/1 10/1 11/1 12/1
spor
es/m
3
Ascospores
0
2000
4000
6000
8000
10000
12000
1/1 2/1 3/1 4/1 5/1 6/1 7/1 8/1 9/1 10/1 11/1 12/1
spo
res/
m3
Cladosporium
0
5000
10000
15000
20000
25000
30000
35000
40000
45000
1/1 2/1 3/1 4/1 5/1 6/1 7/1 8/1 9/1 10/1 11/1 12/1
sp
ore
s/m
3
Alternaria
0
500
1000
1500
2000
2500
1/1 2/1 3/1 4/1 5/1 6/1 7/1 8/1 9/1 10/1 11/1 12/1
spor
es/m
3
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Spore plumes show the influence of environmental conditions
Total Spore Concentration and Wind Speed Hectorville, OK - Sept 21, 1998
0
20000
40000
60000
80000
100000
120000
140000
160000
180000
200000
12:00a.m.
2:00a.m.
4:00a.m.
6:00a.m.
8:00a.m.
10:00a.m.
12:00p.m.
2:00p.m.
4:00p.m.
6:00p.m.
8:00p.m.
10:00p.m.
Time
To
tal S
po
re C
on
ce
ntr
ati
on
s
(sp
ore
s/m
^3
)
0
1
2
3
4
5
6
7
Win
d S
pe
ed
(m
/s)
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Sources of Aerosols
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Point Sources
• Personal (i.e. sneezes, vomitus, etc)
• Natural
• Anthropogenic– Agricultural– Intentional– Industrial
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What are other sources?
• Home IAQ
• Occupational Sources– Healthcare setting– Food processing– Other
• Outdoor Sources
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Factors Affecting Survival of Pathogens in Bioaerosols
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Factors Affecting Bioaerosol Stability
• Temperature
• Humidity
• Composition (moisture, salts, protein, etc.)
• (Sunlight)
• (Wind)
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Stability of Airborne Microbes
• Relative Humidity
• Temperature
• Oxygen
• Open Air Factors (e.g. Ozone, olefins..)
• Radiation (e.g. UV, γ-rays, X-rays)
• Suspending media (salts, proteins, sugars)
• (Air Movement- e.g. wind shear)
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Major Losses of Viability
• Maillard Reactions (dessication)• Membrane phase Changes• Cross linking• Free radical damage (hydroperoxide and
hydroxyl)
• Resulting in – Phospholipid crystalization– Change in permeability barrier function– Energy production capability– Temp. associated death mechanism
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Mobility of Aerosols
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Movement in Air
• Advection
• Mechanical Diffusion
• Molecular Diffusion
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Deposition
• Surface impaction– Essentially a collision between particles and surfaces– Not necessarily permanent
• Rainfall• Electrostatic• Turbulent Diffusion• Thermal gradients• Electromagnetic radiation
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Deposition
• Gravitational Settling– Stokes Law: v= pd2g/18n (cm/sec)
v= velocity, p= particle density, d= particle diameter, g= acceration due to gravity, n=viscosity of airAssumes spherical shape
• For particles>1 micron diffusion due to gravitational settling is dominant
• For particles <0.5 micron, V→→0
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Deposition
• Molecular Diffusion– Tend to be downwardly directed by gravity– Random movements– Highly influenced by wind
• Increases with wind strength
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Brownian Motion
• Bioaerosols are subject to Brownian motion as described by Einstein’s equation
• X=root mean square particle displacement, cm
• t= time, s• r=particle radius
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