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CEE 1503
Air Pollution
Meteorology and Control
Spring, 2005
Meteorology of Air Pollutants
Wind Rose
A Graphical
Picture of
The Direction
And Velocity
From Which
The Wind
Came
Pollution Rose
A Graphical
Picture of
The Direction
And
Magnitude
From Which
The Pollution
Came
Which Plant
Is the
Offending
Plant ?
Plant
Number 3
Lapse Rate
Temperature Change With Height
Adiabatic
No exchange of heat of the parcel of air
under consideration with the outside air.
Given a Known Volume of Air
As the above parcel of air rises,
it experiences less and less pressure
Ideal Gas Law:
PV = nRT
Since the volume stays the same,
the reduction of pressure corresponds to a
lowering of the temperature of the known volume of air.
Dry Adiabatic Lapse Rate
The rate at which non-moist air cools as it rises.
Calculated to Be:
-9.8 oC/km = -5.4 oF/1000 ft = -1 oC/100m
The actual temperature change of the air with
height is the Prevailing Lapse Rate
Lapse Rates
T
T - 1
100 m
Elevation
(m)
Temperature (oC)
Dry Adiabatic Lapse Rate
Lapse Rates
• Superadiabatic, Strong, Unstable
– Temperature Reduction > 1 oC/100m
• Subadiabatic, Weak, Stable
– Temperature Reduction < 1 oC/100m
• Neutral
– Temperature Reduction = 1 oC/100m
• Inversion (Extreme Subadiabatic)
– Temperature Increase with Height
Lapse Rates and
Atmospheric Stability
Atmospheric Stability
Superadiabatic – Strong Lapse Rate
Unstable Conditions
Atmospheric Stability
Subadiabatic – Weak Lapse Rate
Stable Conditions
Lapse Rates and Their
Effect on Smokestack
Plume Shapes
Lapse Rates and Atmospheric Stability
Strong Lapse Condition (Looping)
Wind
Lapse Rates and Atmospheric Stability
Weak Lapse Condition (Coning)
Wind
Lapse Rates and Atmospheric Stability
Inversion Condition (Fanning)
Wind
Lapse Rates and Atmospheric Stability
Inversion Below, Lapse Aloft (Lofting)
Wind
Lapse Rates and Atmospheric Stability
Weak Lapse Below, Inversion Aloft
(Trapping)
Wind
Lapse Rates and Atmospheric Stability
Actual Temperature Sounding
Dispersion Modeling
Predicting Air Pollutant Concentrations
Or
Air Pollution Control by Dilution
Gaussian Dispersion Model
Atmospheric Dispersion Model
• A very simple model based upon Gaussian
diffusion equations
• This type of model is used to model the
atmospheric dispersion of:
– A pulse release in three-dimensions
– A steady-state plume from a continuous source in two-
dimensions.
Dispersion Model Assumptions
• The predominant force is the wind.
• The greatest concentration of the pollutant
molecules is along the plume centerline.
• The process is a steady state process.
Dispersion Model Construction
• Plume travels horizontally in x-direction
• Plume disperses horizontally (y) and vertically (z)
• Concentration inside the plume follows Gaussian
Distribution
• Concentration (C(x,y,z)) is proportional to:
– Source strength (Q)
– Inverse of wind speed (1/U)
– Normalized Gaussian distribution function in the y and z directions
that is dependent on weather conditions
Plume Dispersion Coordinate System
Gaussian Function
G = A e
-0.5(y/y)2
Where,
y = the perpendicular distance from the
centerline of the plume
 y= Gaussian function in the y direction
where the standard deviation in the
y-direction will describe the dispersion
in the y-direction.
Gaussian Dispersion Model
C(x,y,z) = Gy Gz
Q
u
Note:
Atmospheric stability is classified in
categories A through F.
Atmospheric Stability Categories
• A&B = Superadiabatic
• C = Neutral
• D = Subadiabatic
• E = Weak inversion
• F = Strong inversion
Key to Stability Categories
Horizontal Dispersion Coefficients
Vertical Dispersion Coefficients
Effective Stack Height
ON BOARD
Final Model Construction
ON BOARD
The Air Pollution Problem
Emission
Source
Atmosphere Receptors
Pollutants Mixing and Chemical
Transformation
Air Pollution Sampling
and Control
The Air Pollution Control System
Emission
Source
Source
Control
Atmosphere
Detector
Humans
Animals
Plants
Materials
Receptor
Control
Response
Response
Air Pollution Control Strategy
Comprehensive air
pollution control strategy
Long-term control Short-term control
Urban planning
and zoning
Rescheduling
of activities
Programmed
reduction of the
emissions
Rescheduling
of activities
Immediate
reduction in
emissions
Requirements for long-term planning
•Air quality objective
•Airshed model
•Survey of control techniques and their cost
•Meteorological probabilities
Requirements for real-time control
•Air quality objective
•Dynamic modeling
•Rapid communication
•Strict enforcement of measures
Cost and Damage of Air Pollution
Particle Sizes and Measurement
Techniques
High Volume Sampler
Cascade Impactor
Bubbler
Stack Sampling Train Schematic
Gas Sampling Equipment
Air Pollution Control Technologies
• Control of Particulate Emission
- Settling
- Cyclone separation
- Wet scrubbing
- Baghouse filtration
- Electrostatic precipitation
• Control of Vapor-phase Emissions
– Wet scrubbing
– Activated carbon adsorption
– Incineration
Gravity Settling Chamber
Cyclone
Cyclone
Wet Collectors
Wet Collectors
Lime/Limestone Slurry Scrubber System for SO2 Control
CaCO3 + SO2 + H2O  CaSO3 + CO2 + H2O
CaCO3 + 2SO2 + O2 + H2O  2CaSO4 + 2CO2 + 2H2O
Baghouse Filters
Fabric Filters - Baghouses
Fabric Filters - Baghouses
Principle of ESP Operation
Electrostatic Precipitator
Electrostatic Precipitators
Electrostatic Precipitators
Wet ESP
Leonard
W.
Casson,
Ph.D.,
P.E.,
DEE
Wet ESP
Activated Carbon Adsorber
Incinerator
Effectiveness of Particulate Control Technologies
Efficiency of Particulate Control Devices
Efficiency of Particulate Control Devices

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Meteorology 11.ppt