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    Aerobiology

    Microbiology of the Atmosphere

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    Aerobiology

    The interdisciplinary science that deals with

    the movement and dispersal of bioaerosols

    The movement of bioaerosols is generallypassive 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 - 0.5m to 100 m

    Capable of eliciting diseases that may be

    infectious, allergic, or toxigenic with theconditions being acute or chronic

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    Bioaerosols in Our Environment

    Outdoor Sources

    Fungal Spores

    Pollen Bacteria

    Indoor Sources

    Viruses

    Bacteria Fungal Spores

    Dust mites

    Cockroaches Animal Dander -

    especially cats

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    Outdoor Aerobiology

    Atmosphere

    Transport

    Fungal Spores Pollen

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    Spores, Pollen and Gravity

    In still airspores (and pollen) fall to the

    ground at a rate (based on Stokes law)

    that is proportional to the square of itsradius

    i.e. the bigger the spore the faster it will fall

    Aerodynamics also influenced by

    non-spherical shape or irregular shape

    ornamentation and aggregation

    these increase drag and delay deposition

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    Stokes Law

    V =2 s r

    9

    gr2

    V = terminal velocity in cm/s

    s= density of sphere

    r = density of air

    g = acceleration due to gravity

    = viscosity of air )1.8 x 10-4g/cm/sec

    r = radius of sphere

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    0.5 - 14.0

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    Settling rates of particles

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    Airborne Transport

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    Effects of

    environmental

    factorsImpact

    Deposition

    Dispersal

    Take-off

    Source

    The Aerobiological Pathway

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    Airborne Transport

    Perfectly still air seldom occurs

    Prevailing air currents delay deposition by

    gravity

    Air flow is complex allowing bioaerosols to be

    transported over short ranges to global

    distances

    Transport occurs in the turbulent layer of the

    atmosphere

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    Turbulent Layer of Atmosphere

    Air movement shifting and unpredictable

    Depends on wind speed, direction,temperature, and local eddies caused byroughness of the terrain

    Fungal spores are a normal component of

    the turbulent layer possibly up to 200,000spores/m3of air; however, pollen levelsnormally two orders of magnitude lower

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    Long distance transport

    Well documented in palynology literature as

    well as in aerobiology literature

    Typically these are reports of one time

    incursions of exotic pollen types or preseason

    pollen

    Exoticpollen in sediments in Canada

    Preseason birch pollen in Scandinavian countriesfrom southern areas in Europe

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    Well studied examples of long

    distance transport

    Wheat rust sporesStarting in the 1920s the

    movement of Pucciniagraminisspores has

    been demonstrated

    Tobacco blue moldSince late 1980s, themovement of Peronospora tabaccina spores

    has been followed

    Mountain cedar pollenMy lab has been

    following the LDT since 1980

    African dust and associated microorganisms

    have been studied over past decade

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    Juniperus asheipollen

    Juniperus ashei (mountain cedar) has a limiteddistribution Arbuckle Mountains of Oklahoma

    Edwards Plateau of Texas

    Scattered areas of Ozarks

    Highly allergenic (cedar fever in Texas) Tulsa allergist reported 15% patient sensitivity

    Mid-winter pollination (Dec. and Jan.) Tulsa pollen season Feb through early Nov

    Evidence of pollen in Tulsa atmosphere Cedar pollen detected since 1980

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    Juniperus asheigrows amongst the dissected

    slopes of Cretaceous limestone of the Edwards

    Plateau. The species co-occurs withJ. virginiana

    to the east and J. pinchotii otherJuniperus spp. to

    the west.

    Distribution of Juniperus ashei

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    Incursion of J. asheipollen into Tulsa

    Each winter since 1980 J. asheipollen has

    been registered by our Tulsa air samplers

    Pollen recorded on 20% to 60% of the days

    in Dec and Jan

    Concentrations typically low however very

    high concentrations have been registered on

    several occasions (based on NAB level ofvery high >1500 pollen grains/m3)

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    Mountain Cedar Forecasting

    Started in Dec 1998

    Daily forecasts in Dec and Jan

    Forecasts posted on internet athttp://pollen.utulsa.edu

    During past 6 season 812 forecasts issued Three sites in TexasAustin, Junction, San

    Angelo One site in OklahomaArbuckle Mountains

    One site in ArkansasOzark Mountains (5 yrs)

    http://pollen.utulsa.edu/http://pollen.utulsa.edu/
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    Forecast Components

    Release forecastbased on meteorologicalconditions and phenology of the plant Temperatures above 45o F

    R.H. below 50%

    Sunshine

    No rain in previous 24 hours

    Pollen cone maturity

    Downwind forecast based on model projections

    using: HY-SPLIT model trajectories

    Meteorological conditions along the path

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    University of Tulsa

    Mountain Cedar Pollen Forecast

    Date Issued: 15 January 2000

    Mountain Cedar location(s): Arbuckle Mountains, OK

    Regional weather: Friday/Saturday, January 14/15 - TX/OK: High pressure will control

    the weather for the weekend. Moist flow off the Gulf of Mexico is causing some clouds

    and showers in deep South TX and some variable cloudiness in south-central TX.

    Cloudiness will increase today for other parts of southern TX and there may be somedrizzle tonight. Otherwise, fair weather will prevail, and the chance of rain will diminish

    for southern TX as the center of the High moves away to the east. Late-night/early

    morning clouds in some areas Saturday night are expected. Warming trend through the

    weekend. Highs today 50's and 60's, lows tonight 30's to 50's, highs Saturday 60's and

    70's.

    Trajectory weather: Mostly sunny today, high in the 60's. Partly cloudy tonight, low

    near 40. Dry with a high around 60 on Sunday.

    Trajectory confidence: High

    OUTLOOK: *** Serious Threat*** Conditions are favorable for pollen release.

    Strong release expected. Temperatures and humidities are favorable much of the day.

    Airborne pollen will be moving into northeast OK (including the Tulsa area) later

    this afternoon.... and across southern MO and southern IL tonight. Residents of

    western KY may also be affected. TK

    T j t St t( ) ( h b th * ) S lf Okl h

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    Trajectory Start(s)(shown by the *on map): Sulfur, Oklahoma

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    1998-2004 Tulsa Cedar Profile

    During Dec and Jan of the 6 yearscedarpollen present on 233 days

    Most days lowlevels

    Over 50 days moderate to very highlevels 12 days with highlevels

    One day had very highlevel (2,109 pollen/m3)

    Trajectories crossed Tulsa >150 times with

    the majority of trajectories from the ArbuckleMts.

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    London, Ontario

    Air sampling data from Jim Anderson from

    London, Ontario

    Juniperuspollen recorded 22 times in Dec

    and Jan from 1998-2004

    Maximum was 58 pollen grains/m3

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    Continental transport

    27 Jan 99, Jim Anderson inLondon, Ontario reportedatmospheric Juniperuspollen - 58 pollen grains/m3

    Trajectories show that the

    source of this pollen wasTexas population ofJuniperusashei

    Our Jan 26 forecastindicated that the pollenhas the potential to travelvery long distances.

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    Fungal Bioaerosols

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    THE FUNGI

    Kingdom Protista

    Div Myxomycota

    Div Oomycota

    Kingdom Eumycota

    Div Chytridiomycota

    Div Zygomycota

    Div Ascomycota

    Div Basidiomycota

    Asexual Fungi

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    FUNGAL SPORES

    Majority of spore types adapted for airborne

    dispersal

    Spores unicellular to multicellular from 1 to

    100 m

    Main sources in the environment

    Leaf surfaces (phylloplane fungi)

    Soil

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    Spore Release Mechanisms

    Passive

    Wind - generally the most abundant airborne

    spores in the atmosphere - include membersof the Dry Air Spora which peak in afternoon

    Rain - rain splash as well as tap and puff

    Active

    Generally require moisture

    Common mechanism for ascospores and

    basidiospores

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    Wind Dispersed Spores

    Frequently related to wind speed and

    turbulence

    Typically borne on erect conidiophores or

    sporangiophores that elevate spores above

    the substrate

    Dry Air Spora Cladosporium, Alternaria,

    Epicoccum, Drechslera, Pithomyces,Curvularia, smut spores

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    Dry Air Spora

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    Diurnal Rhythm of Cladospor ium

    Hourly CladosporiumLevels

    Tulsa May 24, 1999

    0

    5,000

    10,000

    15,000

    20,000

    25,000

    30,000

    12:00

    AM

    2:00

    AM

    4:00

    AM

    6:00

    AM

    8:00

    AM

    10:00

    AM

    12:00

    PM

    2:00 PM 4:00 PM 6:00 PM 8:00 PM 10:00

    PM

    S

    pores/m3

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    Cladospor iumspores 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

    Spores/m3

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    Cladospor ium

    Common fungal genusoccurring both indoorsand outdoors

    Most abundant outdoorspore type with aworldwide distribution

    Normally exists as asaprobe or weak plant

    pathogen Spores are known to be

    allergenic

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    Cladospor iumspp.

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    Passive Discharge during Rain

    Vibration and shaking as raindrops hit leaf

    May explain increases in Cladosporium

    during rainfall

    Release of basidiospores by puffballs shows

    similar puffing when raindrop strikes mature

    fruiting body

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    Rain Splash

    Generally spores surrounded by mucilage

    Mucilage protects from desiccation but also

    prevent dispersal by wind

    First raindrops dissolve mucilage

    Resulting spore suspension dispersed by

    subsequent raindrops

    Spores commonly thin, colorless, elongate

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    Active Discharge - Ascospores

    Hygroscopic material within ascus absorbs

    moisture

    Ascus swells and develops high osmotic

    pressure

    Pressure causes ascus to burst, explosively

    shooting spores into the atmosphere

    Need for rainfall will often override diurnalrhythm of release

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    Basidiospore discharge

    from basidium

    Moisture condense around

    crystal of manitol

    Bullers drop enlarges

    Fuses with a film of water

    around spore

    Shifts center of gravity

    Result of discharge

    Spores shot only a fractionof a millimeter

    Spores freed from gill or

    pore and able to fall free

    and reach turbulent layer

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    Basidiospore Rhythm

    Need for moisture

    confines spore release

    to periods of highhumidity

    Typically peak levels in

    pre-dawn hours and

    low levels in afternoon

    May of 1998

    0

    500

    1000

    1500

    2000

    2500

    2:00AM

    4:00AM

    6:00AM

    8:00AM

    10:00AM

    12:

    00PM

    2:

    00PM

    4:

    00PM

    6:

    00PM

    8:

    00PM

    10:

    00PM

    12:00AM

    spores/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

    J F M A M J J A S O N D

    Spores/m3

    0

    10,000

    20,000

    30,000

    40,000

    50,000

    60,000

    J F M A M J J A S O N D

    Spores/m3

    2002

    23 T id tifi d Cl d i A

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    23 Taxa identified: Cladospor ium, Ascospores,Basidiospores, and Alternar iaComprised 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 1 1/1 12/1

    spores/m3

    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

    spores/m

    3

    Cladospor ium

    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

    spores/m3

    A l t ernari a

    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

    spores/m3

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    Indoor Aerobiology

    Outdoor spores enter readily

    Many fungi can also amplify indoors

    anytime moisture is available fungi can grow

    on many indoor substrates

    Penicillium, Aspergillus,andCladosporium

    are most common indoors

    Many can form mycotoxinsAspergillussppand Stachybotrys

    E i t l f t th t i fl

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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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    Typical Yearly Spore Levels 1998

    0

    10,000

    20,000

    30,000

    40,000

    50,000

    60,000

    J F M A M J J A S O N D

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    Spore plumesshow 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

    12:00

    a.m.

    2:00

    a.m.

    4:00

    a.m.

    6:00

    a.m.

    8:00

    a.m.

    10:00

    a.m.

    12:00

    p.m.

    2:00

    p.m.

    4:00

    p.m.

    6:00

    p.m.

    8:00

    p.m.

    10:00

    p.m.

    Time

    Tota

    lSporeConcentration

    s

    (spores/m^3)

    0

    1

    2

    3

    4

    5

    6

    7

    WindSpeed(m/s)

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    Water Leak

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    Humidity

    Indoor relative humidity Below 30% R.H. no mold growth

    Above 70% optimal for mold

    Usually mold growth can occur above 50% Humid air condenses on cool surfaces

    Cold windows in winter - molding and sills become wetand suitable for fungal growth

    Cold floors in winter

    Cooling coils in AC units in summer Humid air allows hygroscopic materials to absorb

    water

    Hi h h idit i h h

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    High humidity in home where

    subslab ducts failed

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    Moisture Problems

    Become worse in past 20 - 30 yrs

    increased use of washing machines, dishwashers

    vaporizers and humidifiers actively spray droplets

    into the air (often contaminated)

    tighter buildings for energy conservation trap

    moisture

    Anytime moisture available fungi will grow

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    Cladosporium one of the most common

    indoor fungi growing on a diffuser

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    Penic i l l ium

    One of the mostcommon soil fungi innatural environment

    Over 250 species

    Well known allergen

    Some species producemycotoxins

    Some species produceantibiotics

    Produce VOCs

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    Penic i l l ium in culture

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    Aspergi l lus

    Also common soil fungi

    Cause rot of stored grain

    Over 150 species

    Well known allergens

    Several species form

    mycotoxins

    Some species can grow at

    high temperatures

    Several species causeinfections in lung, sinuses,

    and hypersensitivity

    pneumonitis

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    Aspergi l lus niger

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    Asperg i llus fum igatus

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    Penic i ll ium and Asperg i llus

    Small spores passively

    aerosolized when spore

    clusters disturbed

    Spores extremely buoyant,remain airborne for

    extended time

    PenicilliumandAspergillus

    spores look alikedistinguished in culture

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    Stachybotrys chartarum

    Soil fungus in nature

    Commonly found indoors on

    wet materials containing

    cellulose, such as

    wallboard, jute, wicker,straw baskets, and paper

    materials

    Spores in slimy mass

    Thought to be allergenicalthough little is known

    May produce potent

    mycotoxins

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    Indoor air sample

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    Air SamplingTechniques

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    Principal Collection Methods

    Gravity

    Impaction

    Impingement

    Filtration

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    Gravity

    Simplest but least accurate method ofcollecting airborne biological samples

    Coated microscope slide or open petri dish

    containing agar exposed to atmosphere Non quantitative for atmospheric

    concentrations

    Affected by particle size and shape and airmovement

    Biased deposition of large particles

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    IMPACTIONSAMPLERS

    Separate particles from the air stream by

    using inertia of particles

    Forces deposition onto a solid or agar

    surface

    Most commonly used method

    Instruments available for culturable sampling

    and total spore sampling

    Impaction Samplers

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    Impaction SamplersTotal Spore Samplers

    Outdoor Samplers

    Hirst Spore TrapBurkard and others

    Rotorod Sampler

    Samplair MK-3 Sampler

    Indoor Samplers

    Burkard Continuous Recording Air Sampler

    Samplair MK-3 Sampler

    Burkard Personal Volumetric Sampler

    Air-O-Cell Sampler

    Cyclex-D Sampler

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    Burkard Spore Trap

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    Advantages of Burkard Spore Trap

    High efficiency down to less than 5 m

    Allows for accuracy for small fungal spores such

    as basidiospores and small ascospores

    Time discrimination Permits analysis for diurnal rhythms

    Permanent slides for future reference

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    Burkard 7-day sampler head

    Standard is the 7-day sampling head

    Sampler drum mounted on 7-day clock

    Drum moves by orifice at 2 mm per hr

    Melenex tape mounted on drum and greased(Lubriseal, High Vacuum Grease, other)

    Air is brought in at 10 l/min and impacts on greased

    Melenex tape

    Drum changed each week

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    Seven Day Sampling Head

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    Processing the 7-day drum

    Melenex tape removed from drum

    Tape cut into seven 24 hour segments each 48 mmlong

    Segments mounted on microscope slides in 10%gelvatol (polyvinyl alcohol) and dried

    Glycerin-jelly mounting medium added and a 50 mmcover slip

    Mounting medium contains pollen stain - either basicfuchsin or phenosafarin

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    Melenex tape on cutting board

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    24 hour sampling head

    Outdoor Air Sample from Burkard Spore Trap

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    Outdoor Air Sample from Burkard Spore Trap

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    Rotorod Samplers

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    Rotorod Samplers

    Models most often used have retracting rodsfor intermittent operation (10% sampling timetypical)

    Head rotates at 2400 rpm Leading edge of rod coated with grease

    Pollen and spores impacted on greasedsurface

    Efficient for pollen and spores >10 m

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    Rotorod Sampler

    Rods spin at 2400 rpm. Particles (spores and pollen) are impacted on

    leading face of the rod which is greased. Efficiency decreases dramatically

    below 10 m. Intermittent head spins 10% of time.

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    Allergenco Samplair

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    Continuous Recording Burkard

    24 hour sampling onto a coated microscope slide

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    Burkard Personal Sampler

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    Air-O-Cell Slide

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    Cyclex-d

    Andersen (N-6) Single Stage

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    ( ) g g

    Sampler

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    Andersen 6-Stage and 2-Stage Impactors

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    Biocassette Sampler

    Burkard Portable Air Sampler for Agar

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    Burkard Portable Air Sampler for Agar

    Plates

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    Inpingement Samplers

    Separate particles from the air stream by

    using inertia of particles

    Forces deposition into liquid collection

    medium (usually a dilute buffer)

    Aggregates of cells can be broken apart

    Allows for several possible analytic

    applications: culture, microscopy,biochemistry, immunoassays, PCR

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    Impingers

    AGI-30 BioSamplerBurkard

    Multi-stage

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    Filtration

    Separates particles from airstream by

    passage through a porous substrate, usually

    a membrane filter

    Collection depends on filter pore size andflow rate

    Loss of viability may occur due to desiccation

    Adaptable for a variety of assays

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    Sampler Performance

    Collection efficiency is the ability to capture

    the particles onto the collection medium

    Physical characteristics of the inlet and the

    airflow rate used to calculate d50 Particle diameter at which 50% of particles are

    collected

    Because of sharp cut-off it is generally acceptedthat all particles above this size are collected

    d50 values for some samplers (CUT SIZE)

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    d50values for some samplers (CUT SIZE)

    Sampler d50

    AGI-30 Impinger 0.30 m

    Air-O-Cell Cassette 2.30 m

    Andersen Single Stage 0.65 m

    BioSampler Impinger 0.30 m

    Burkard 7-Day Spore Trap 3.70 m

    Burkard Personal Sampler 2.52 m

    Buttner MP, Willeke K, Grinshpun SA. Sampling and Analysis of Airborne

    Microorganisms. In: Manual of Environmental Microbiology 2nded. ASM Press,

    Washington, 2002.

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    Analytic Methods

    Microscopy

    Culture

    Biochemistry Molecular Biology

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    Microscopy

    Identification of total spores (both culturable

    and non-culturable) along with pollen and

    other particulates

    Identification to species level usually notpossible

    Identification of morphologically similar

    spores not possible

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    Culture

    Only viable bacteria and fungi

    Limited to those taxa able to grow in culture

    on medium used

    Success based on medium and incubation

    time and temperature

    Permits speciation when required

    Results expressed as CFU/m3

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    Biochemistry

    Detection of specific compounds

    May not be specific for a genus or species

    Assay examples:

    Ergosterol

    B 1,3-glucan

    Endotoxins

    MycotoxinsStachybotrys toxins and ochratoxin

    Various types of assays such as HPLC

    I h i

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    Immunochemistry

    Specific allergen molecules

    Not useful for routine air sampling

    Typically used for filter samples and impinger

    samples but have been used for spore trapsamples

    Requires prior development of an antibody

    Widely used for dust mite, cockroach, cat,etc.

    Few fungal assays available

    M l l Bi l

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    Molecular Biology

    Detection of specific genetic elements

    Highly specific and sensitive

    Currently restricted to a few organisms