Title: Chapter 5 Dispersion Models
1Chapter 5 Dispersion Models
- 5.1 Dispersion of pollutants in the atmosphere
- 5.2 Models
- 5.3 Gaussian Dispersion Model
- 5.4 Effective stack height
- 5.5 Area and line sources
2Introduction
- Connection between Source and Atmosphere
- Emissions of pollutants from sources
- Air quality in the atmosphere
- Emission ?Air Quality (Imission)
- Connection MODELS
- Very wide variety of models
3What is MODEL?
- A mathematical relation (equation or a set of
equations) to estimate some parameter(s) (i.e.
Outputs) by using some other set of parameter(s)
(i.e. Inputs)
MODEL Yj f(Xi)
Output(s), Yj
Input(s), Xi
4MODELS
- Deterministic ModelsInitially KNOWN relationship
between inputs and outputs - Box Models (Simple Box Model, Eulerian Box
Model, Lagrangian Box Model) Receptor
Models Dispersion Models
5MODELS
- Stochastic Models
- Initially UNKNOWN relationship between inputs
and outputs - Mathematical approximations such as polynomial
equations, neural networks, fuzzy networks etc
6General Structure of Air Pollution Models
7Detailed Structure of Atmospheric Chemical
Transport Models
8Parameters in Models
- Source Parameters (Emission Characteristics) Emis
sion rates of pollutants (mass/time) Physical
location of source Temperature of gas
release Plume Rise - Meteorology Atmospheric temp. Atmospheric
stability (needed for Dipersion coefficients)
Wind velocity - Atmospheric Chemistry Chemical Reaction in the
atm. Depositions (wet or dry) - Surface Parameters Surface geometry, roughness,
seas, urban or rural areas etc
9Scope of this Chapter
- Dispersion Models
- GAUSSIAN DISPERSION MODEL
10Theory Behind Gaussian Dispersion Model (GDM)
- A Mass Balance on the basis of a specific
pollutant In a Control Volume - Accumulation Rate (mass/time)
- All Flows In
- All Flows Out
- Formation Rate
- - Destruction Rate
11Theory Behind Gaussian Dispersion Model (GDM)
Inputs
Diffusion
Outputs
Advection (by wind)
- Two main transportation mechanisms are involved
- Diffusion on molecular basis in all directions
(i.e.in x, y and z directions) - Transportation by wind in only wind direction
(i.e. in x direction)
12Theory Behind Gaussian Dispersion Model (GDM)
- Molecular diffusion
-
(Ficks Law) - Nx Mass diffusion flowrate of gas pollutant in
x direction (mass/time) - Dx Diffusivity (turbulent mixing coefficient)
in x direction (area/time) - C Concentration (mass / volume)
- A Cross-sectional area (Adydz) in the
direction of transportation (i.e. x direction)
13Theory Behind Gaussian Dispersion Model (GDM)
Ci concentration of pollutant i, µg/m3 u
mean convective velocity in x-direction (wind
velocity), m/sec dy mean convective velocity
in y-direction, m/sec dz mean convective
velocity in y-direction, m/sec Dx mass
diffusivity in x-direction, m2/sec Dy mass
diffusivity in y-direction, m2/sec Dz mass
diffusivity in z-direction, m2/sec F pollutant
removal or accumulation rate, µg/sec
14Theory Behind Gaussian Dispersion Model (GDM)
Dividing both sides by control volume dxdydz
Assuming mass diffusivities are constant due to
continuity principle, that is
15Theory Behind Gaussian Dispersion Model (GDM)
- Last equation becomes
- Basic dispersion equation
- We need to evaluate Gaussian Dispersion mechanism
to further go on
16Gaussian Dispersion Mechanismin 2D
17Gaussian Dispersion Mechanismin 3D
18Gaussian Dispersion Mechanism
- In order to obtain Gaussian Model, we need to
simplify the Basic dispersion Equation - Assumptions
- Pollutant emission rate (Qi) from the source is
constant - Wind velocity in y and z directions is zero
- Wind velocity in x direction is constant
- Advective transportation is dominant over
diffusion in x direction
19Gaussian Dispersion Mechanism
- Pollutant accumulation or removal is zero
- F0
- With all these assumptions Basic Eqn
- Becomes a second order differential eqn
20Gaussian Dispersion Mechanism
- Solution
- K is an indefinite integration constant
- To find K we need to determine the integration
limits depending upon the dispersion geometry. - In the plume we have
21Gaussian Dispersion Mechanism
- Integration limits for a ground source
- y -infinity to infinity
- z 0 to infinity
- Result
- K is
22Gaussian Dispersion Mechanism
- Inserting into main eqn
- By definition we have the following relations
between diffusion and dispersion coefficients - Inserting them into main eqn,we have
- Gauss Dispersion Eqn for ground level source
23Concepts about GDM
24Concepts about GDM
- Stack Dip Downwash
- If
- Stack dipdownwash is neglected
- Otherwise Reduced Stack height
25Concepts about GDM
26Concepts about GDM
27Concepts about GDM
28Concepts about GDM
- Ground Reflection
- (Vertical Concentration profile)
29Concepts about GDM
- Ground Reflection
- (Horizontal concentration change)
Cmax and its location (xmax) is important
30Most General Form of GDM
31Plume Shapes depending on Stability
32Plume Shapes depending on Stability
33Plume Shapes depending on Stability
34Plume Shapes depending on Stability
35Plume Shapes depending on Stability
36Plume Shapes depending on Stability
37How to use GDM?
- Need to know proper orientations of both Source
and ReceptorSource at (0,0,H) and Receptor at
(x,y,z) ?C(x,y,zH) - Pollutant Emission Rate from source Q (mass of
pollutant/time) NOT Volume flowrate of
Stackgas - Atmospheric Stability Category (A, B, C. etc.)
- Wind velocity at stack height u
- Dispersion Coefficients sy and sz
- Effective Stack height H hs ?h ?
Calculation of Plume rise (?h ) - THEN USE GDM ? C(x,y,zH) .
38Source-to-Receptor Orientation
- A source is emitting pollutant stack gas from its
stack of 100m. Define the location of a ground
level receptor site 5 km North (N) of the source
if the wind blows from SouthWest (SW) direction. - ?Draw the geographical orientation of source and
receptor and calculate x, y and z coordinates
for GDM.
39Distance x (5 km) Cos 45
40Receptor-to-Source Orientation
- A park area is located in 10 km west (W) of a
thermal power plant having 200m tall stack.
Determine the geographical positions of receptor
and source points if the wind blows from
East-NorthEast (ENE) direction. - ?Draw the geographical orientation of source and
receptor and calculate x, y and z coordinates
for GDM
41 42Dispersion Coefficients sy, sz
As plume goes away from source, dispersion
increases in both y and z directions ? As x
increases ? sy and sz icrease depending upon
stability
43Dispersion Coefficients sy, sz
- First developed graphical representations
sy
sz
44Dispersion Coefficients sy, sz
- Mathematical simulations for Disp. Coeffs.
45Calculation of Plume Rise (?h)
46Calculation of Plume Rise (?h)
47Calculation of Plume Rise (?h)
48Calculation of Plume Rise (?h)
49Calculation of Plume Rise (?h)
- Parameters in Briggs Equations
50EXAMPLES
51EXAMPLES
52EXAMPLE
53Graphical representation of concentration versus
x distance
54Ground Level Max Concentration and Location
- Turners Graphical Solution
- A Graph for
- Cu/Q versus xmax
- Max Concentration depends on
- Stability category
- Effective stack height
- GRAPH
55(No Transcript)
56Analytical Solution for Cmaxvalid for all
stability categories
57Analytical Solution for Cmaxvalid only for
Slightly stable and Neutral conditions