Calculate pollutant dispersion using Gaussian plume model. Estimate ground-level concentrations based on emission sources and meteorological conditions.
| 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 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.
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:
| 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 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 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 |
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.