Introduction to Aerobiology : Origin, Sources, Fate and Transport of Air Pollutants Prof. Mukesh...
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Transcript of Introduction to Aerobiology : Origin, Sources, Fate and Transport of Air Pollutants Prof. Mukesh...
Introduction to Aerobiology : Origin, Sources, Fate and Transport of Air Pollutants
Prof. Mukesh KhareDepartment of Civil Engineering
Indian Institute of Technology DelhiE-mail ID: [email protected]
International Perspectives on Quantitative Microbial Risk Assessment
IIT Delhi Summer School 2014
What is Aerobiology? Bio-aerosols/characteristics Sources of bio-aerosols Bio-aerosols: stability Bio-aerosols: fate and transport Fate and transport modelling techniques ADMS modelling techniques Application in Aerobiology Building assessment References
Overview
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The study of the sources, dispersion, and effects of airborne biological materials, such as pollen, spores, and microorganisms.
The movement of bioaerosols is generally passive and is greatly influenced by the surrounding environment.The viability of bioaerosols is dependent on the environmental conditions.
What is Aerobiology?
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Mixture of solid or liquid particles in air containing whole or part of biological materials
Biological materials include human pathogens, toxic or allergic pieces of microorganisms, dust mite parts or feces, animal dander, fur, dried saliva and animal waste products
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 organisms
Particle sizes: typically 0.5µm to 100µm. Generally assumed having properties of gases.
Capable of eliciting diseases that may be infectious, allergic, or toxigenic with the conditions being acute or chronic
Bio-aerosol: Characteristics
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Bio-aerosol: Sources
Natural sources Pollen (Part of the life cycle of plants) Spores (Part of the life cycle of fungi) Microorganisms/plant Substances from of animals
Anthropogenic sources Indoor Air: Damp and mouldy buildings Laboratory activities Recycling facilities (e.g. composting) Intensive mass animal farming Human
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Physical Sunlight Open air factors (e.g. ozone) Air movement (e.g. wind shear)
Biological Oxygen Radiation (e.g. UV, Ƴ-rays, X-rays) Suspended media (salts, proteins, sugars)
Environmental Temperature Relative Humidity Composition (moisture, salts, protein, etc.)
Bioaerosol: Stability
Source: ACGIH, 1999 IIT Delhi Summer School 2014
The movement, motion, dissemination and equilibrium in the environment fall in category of fluid mechanics.
Bioaerosol: Mobility
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Molecular scaleThe motion is called Molecular Diffusion
Ex- Diffusion within sediments
Global scaleThe motion is called Dispersion
Ex- Transport of gases and aerosols by large air masses
Scale of Motion
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What is Flux ?Mass of diffusing particles/gases crossing unit area in unit time in direction of motion.
Motion of the pollutants is accomplished by flux of that pollutant.
Pollutant flux = f (Mass flux, Dispersion flux, Diffusion flux, Source, Sinks)
The Flux
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Advection x
yz
Turbulent Diffusion
Turbulent Eddies
x
zy
Dispersion
a
b
c
Advection, Diffusion & Dispersion
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Atmospheric Turbulent Flows
Dissipation Dispersion RandomFluctuations
Mixing and KEDissipates depending upon the density stratification in the atmosphere
Diffusion and Advection
Case A: If Density of lower layer of air > Density of upper layers
Case B: If Density of lower layer of air < Density of upper layers
Case B: Applicable to atmosphere in day time
Case A: Applicable to atmosphere during night timeReduced
Enhanced
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The Dispersion
Source ReceptorTransport
Re-entrainment
Source : Point, Line, AreaReceptors : HumansTransport : Fate of air pollutantsRe-entrainment : Re-suspensions of air pollutants
Dispersion = Advection (Transport) + Dilution (Diffusion)
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The Diffusion: Types
Nomalous
Molecular/Brownian
Diffusion
Anomalous
Atmospheric
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The Diffusion Equation: Basic
c = + ; ui = + ’
= 0 ; = 0
Conservation of mass principle In Cartesian coordinate, C = C(x, t) It neglects small terms due to molecular diffusivity
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The Gaussian Diffusion Equation
Analytical solutions to the diffusion equation
Simplest case: One dimensional (In the z - direction)Vertical diffusion (Kz) = constant
Mean wind speed () = x/t
(z, t) e^[- (1/2) * (z/ )2]
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System approach to air quality model
A relationship between emissions and air quality that incorporates the transport, dispersion and transformation of compounds emitted into the air.
What is Air Quality Model?
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Three step process:i. Pre-processor : emission data- micro-organism
characteristics, emission rates, meteorological data, grids, emitter coordinates etc.
ii. Processor : Gaussian based dispersion model, settling velocity etc.
iii.Post-processor: Micro-organism concentration map, frequency map etc.
Bio-aerosol Modelling
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Emission: Release of air pollutants into the atmosphere which are put into the air or emitted by various sources.
Emission Inventory (EI): A list of the amount of pollutants from all sources entering the air in a given time period. The boundaries of areas are fixed.
The Emission
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Why emission inventory (EI) is needed?
For planning and zoning the area study.EI can point out major sources.EI is helpful in deciding control strategies.EI is used in mathematical models to determine the
degree of overall control necessary to meet ambient air quality standards.
EI can be used to indicate type of sampling network and location of monitoring station.
Contd….
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SBER Measurement
Portable Wind Tunnel
Schematic diagram of wind tunnel (Case study)*
Reference: Taha, M.P.M., Pollard, S.J.T, Sarkar, U., Longhurst, P. (2005). Estimating fugitive bio-aerosol releases from static compost windrows: feasibility of portable wind tunnel approach. Waste Management, 25 (4), 445-450.
Note: Only baseline fugitive emission are measured. No other influencing factor are considered.
SBER/A
whereSBER= specific bio-aerosol emission rate (cfu/m2/s);Q = flow rate through the wind tunnel (m3/s);BC = bio-aerosol concentration in air (cfu/m3); andA= area covered by the wind tunnel (m2)
SBER = f { Source material, outside condition/process, individual bio-aerosol properties, geographical, topographical and meteorological condition}
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The Meteorology
Atmospheric Characteristics
Meteorology is the interdisciplinary scientific study of the atmosphere that focuses on weather processes and short term forecasting (in contrast with climatology).
Characteristic of atmosphere is its ability to resist vertical motion: Stability
Affects atmospheric ability to disperse pollutants When parcel of air is displaced upward
Encounters lower pressure Expands to lower temperature Assume no heat transfers to surrounding atmosphere
(adiabatic)IIT Delhi Summer School 2014
Different variables affecting air pollutants transport of diffusion in the atmosphere are:
a) Wind speed and directionb) Vertical temperature gradient (lapse rate)c) Stability of the atmosphered) Roughness element of the earth surfacee) Humidity or water vapor in the atmospheref) Solar radiation
Contd….
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Wind speed profile with height
Contd….
u p
u1 = reference wind velocity at 10m; z1 = reference height of 10m; p =depends upon stability and surface configuration
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Wind direction profile with heightZ
Y
X
Z
Y
X
Circular plume [a=b] Elongated plume [a>b]
Wind direction changes with height It produces crosswind horizontal shear – this increases the
horizontal dispersion
Contd….
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Rate of change of temperature of the parcel of air (smoke) with height.
Types of Lapse Rate ( dT/dz)Dry Adiabatic Lapse rate (Гd) : - 1°C/100m or (DALR) - 5.4°F/1000ftSaturated Adiabatic Lapse Rate (Гsat) : -0.60C/100m
(SALR)Environmental Lapse Rate: Actual change in
temperature of the (ELR) surrounding environment
Lapse rate (Г)
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• Comparison of Γd to ELR classifies stability of atmosphere.
• Degree of stability is a measure of the ability of the atmosphere to disperse pollutants
Significance of Lapse Rate
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Cambridge Environmental Research Consultants3, King’ s Parade, Cambridge CB2 1SJ, UK
Telephone : +44 -1223357773Email: [email protected]
Website : http://www.cerc.co.uk
Emission rate
Management Practices
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• Atmospheric Dispersion Modeling System• Can be use for Point, Line, Area, Volume,
Grid sources• Can model for continuous as well as discrete
point source• Flat or complex terrain• Multiple buoyant industrial emissions• Urban or rural areas• Valid to 60km, useful to 100 km
Model Features
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Integrated meteorological pre-processor, choice of met input parameters like cloud cover, surface sensible heat flux, radiation.
Can input albedo and Bowen ratio. Integrated processing for buildings, complex
terrain. Utility to convert US met data to ADMS format,
including AERMOD data. Wet and dry deposition. Time varying source parameters.
Contd…
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Salient Point• Bioaerosol are modelled as particles • Passive particles• Dry deposition • Agglomeration of particles • Gaussian distribution
SOURCE: G.H. DREW, A. TAMER, M.P.M. TAHA, R. SMITH, P.J. LONGHURST, R. KINNERSLEY and S.J.T POLLARD (2006), “Dispersion of Bioaerosols from Composting Facilities”, Proc. Waste Conf. Integrated Waste Management and Pollution Control. Stratford-upon-Avon, UK, 19-21 September 2006.
Application in Aerobiology
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References ACGIH. Bio-aerosols: Assessment and Control. American Conference of Governmental
Industrial Hygienists, Cincinnati, OH. 1999. Aerotech Laboratories, Inc. IAQ Microbial Reference Guide, IAQ Tech Tips,
www.aerotechlabs.com. 2000. ASTM. Biological Contaminants in Indoor Environments. Morey/ Feely/ Otten ed. STP
1071, Philadelphia, Pennsylvania. 1990. G.H. DREW, A. TAMER, M.P.M. TAHA, R. SMITH, P.J. LONGHURST, R. KINNERSLEY and S.J.T
POLLARD (2006), “Dispersion of Bioaerosols from Composting Facilities”, Proc. Waste Conf. Integrated Waste Management and Pollution Control. Stratford-upon-Avon, UK, 19-21 September 2006.
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