SO₂
NO₂
PM₁₀
PM₂.₅
CO
O₃
Custom

Emission Source Parameters

g/s
m
m
m/s
°C
°C

Meteorological Conditions

m/s
° (from North)
A (Very Unstable)
B (Unstable)
C (Slightly Unstable)
D (Neutral)
E (Slightly Stable)
F (Stable)
m

Receptor Location

m
m
m
m (z₀)
Calculating...
Pollution Dispersion Results
42.5 μg/m³
Ground-Level Concentration
1,250 m
Maximum Impact Distance
58.7 μg/m³
Maximum Concentration
Moderate
Air Quality Impact

Pollution Concentration Map

Low Concentration
Moderate
High
Very High

Dispersion Parameters

Parameter Value Units Description
Effective Stack Height 68.3 m Stack height + plume rise
Plume Rise 18.3 m Additional height due to buoyancy/momentum
σy (Horizontal Dispersion) 124.5 m Standard deviation of horizontal distribution
σz (Vertical Dispersion) 78.2 m Standard deviation of vertical distribution
Maximum Concentration Distance 850 m Distance where maximum concentration occurs
Critical Wind Speed 4.2 m/s Wind speed producing maximum concentration

Air Pollution Dispersion Fundamentals

Air pollution dispersion modeling is the mathematical simulation of how air pollutants disperse in the atmosphere. It is used to predict pollutant concentrations at specific locations based on emission sources and meteorological conditions.

Key Application: Dispersion models are essential for environmental impact assessments, regulatory compliance, emergency planning, and air quality management.

Gaussian Plume Model

The Gaussian plume model is the most commonly used air pollution dispersion model. It assumes that pollutants spread in a Gaussian (normal) distribution in both the horizontal and vertical directions.

The basic Gaussian plume equation for ground-level concentrations is:

C = [Q / (2πuσyσz)] × exp[-0.5(y/σy)²] × exp[-0.5(H/σz)²]

Where:

Air Quality Standards

Pollutant Averaging Time Standard Units
PM₂.₅ 24-hour 35 μg/m³
PM₂.₅ Annual 12 μg/m³
PM₁₀ 24-hour 150 μg/m³
O₃ 8-hour 70 ppb
NO₂ 1-hour 100 ppb
SO₂ 1-hour 75 ppb
CO 8-hour 9 ppm

Atmospheric Stability Classes

Atmospheric stability significantly affects pollutant dispersion. The Pasquill-Gifford stability classes are commonly used:

Class Description Conditions Dispersion
A Extremely Unstable Strong solar radiation, light winds Rapid vertical mixing
B Moderately Unstable Moderate solar radiation Good vertical mixing
C Slightly Unstable Slight solar radiation Moderate vertical mixing
D Neutral Overcast or strong winds Neutral conditions
E Slightly Stable Thin overcast, light winds Limited vertical mixing
F Moderately Stable Clear night, light winds Poor vertical mixing

Plume Rise Calculations

Plume rise is the additional height gained by a plume due to its momentum and buoyancy. Common plume rise formulas include:

Formula Application Equation
Briggs General purpose Δh = 1.6 F1/3 u-1 x2/3
Holland Simple estimation Δh = (vs d / u) (1.5 + 2.68×10-3 P ΔT d / T)
Concave Buoyant plumes Δh = 3.0 (F / u)3/5 x2/5

Model Limitations

While Gaussian models are widely used, they have several limitations:

Model Selection: For complex situations (complex terrain, coastal areas, reactive pollutants), more sophisticated models like CALPUFF, AERMOD, or CFD models may be more appropriate.