Adiabatic - No exchange of heat of the parcel of air under consideration with the outside air.
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
7. 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.
8. 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
9. Lapse Rates
T
T - 1
100 m
Elevation
(m)
Temperature (oC)
Dry Adiabatic Lapse Rate
10. 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
24. 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.
25. 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.
26. 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
28. 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.
38. The Air Pollution Control System
Emission
Source
Source
Control
Atmosphere
Detector
Humans
Animals
Plants
Materials
Receptor
Control
Response
Response
39. 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