Air Quality Dispersion Back
Air Quality

Gaussian Plume Air Quality Dispersion Model

Pasquill-Gifford stability classes A–F with Briggs plume rise. Real-time ground-level concentration maps, C_max, and x_max for stack emission scenarios.

Parameters
Presets
Emission rate Q
Stack height H
Exit velocity vs
Stack diameter ds
Wind speed u
Stack gas temp Ts
Ambient temp Ta
Stability class
Terrain
Receptor distance x_r
Results
C_max (μg/m³)
x at C_max (km)
Receptor C (μg/m³)
Plume rise Δh (m)
Top View — Concentration Color Map (x-y)
Side View (x-z)
Ground-level C vs Downwind Distance
σy, σz vs Distance
Theory & Key Formulas
$$C(x,y,z) = \frac{Q}{2\pi\sigma_y\sigma_z u}\exp\!\left(-\frac{y^2}{2\sigma_y^2}\right)\!\left[\exp\!\left(-\frac{(z-H)^2}{2\sigma_z^2}\right)+\exp\!\left(-\frac{(z+H)^2}{2\sigma_z^2}\right)\right]$$

Briggs plume rise: $\Delta h = \dfrac{1.6\,F_b^{1/3}\,x^{2/3}}{u}$, buoyancy flux $F_b = g\,v_s\,(d_s/2)^2\,(T_s-T_a)/T_s$

Regulatory Comparison
WHO PM2.5 annual: 5 μg/m³
Japan PM2.5 annual: 15 μg/m³
Run calculation to assess

What is Gaussian Plume Dispersion?

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What exactly is this simulator modeling? I see a smokestack and a colored plume on the ground.
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Basically, it's predicting how air pollution from a factory stack spreads downwind. The colored map shows the ground-level concentration. The core idea is that turbulence in the atmosphere spreads the plume in a predictable, bell-shaped (Gaussian) pattern in both the horizontal and vertical directions. Try moving the "Wind Speed" slider to see how a stronger wind dilutes the pollution faster.
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Wait, really? The stack height is fixed, but the plume seems to start higher up. What's going on?
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Good observation! That's "plume rise." The hot, fast gas exiting the stack has momentum and buoyancy, so it rises further before leveling off. The simulator uses Briggs' formulas to calculate this effective height. For instance, increase the "Exit Velocity" or "Stack Gas Temp" parameters above—you'll see the plume start higher and reduce ground-level pollution significantly.
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So the "Stability Class" dropdown is super important? What does "Pasquill F" mean in practice?
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Exactly. It describes atmospheric turbulence. "F" stands for "stable" conditions—think of a calm, clear night. The air resists vertical mixing, so the plume stays narrow and can travel far before touching down. Switch to "A" (very unstable, sunny afternoon) and watch the plume spread vertically immediately, causing a higher but more localized peak at the ground. This is a key factor in environmental assessments.

Physical Model & Key Equations

The cornerstone is the Gaussian Plume Equation. It calculates the pollutant concentration at any point (x,y,z) downwind, assuming the plume spreads in a statistically normal (Gaussian) distribution. The model includes a reflection term to account for the ground, which prevents material from dispersing downward indefinitely.

$$C(x,y,z) = \frac{Q}{2\pi\sigma_y\sigma_z u}\exp\!\left(-\frac{y^2}{2\sigma_y^2}\right)\!\left[\exp\!\left(-\frac{(z-H_e)^2}{2\sigma_z^2}\right)+\exp\!\left(-\frac{(z+H_e)^2}{2\sigma_z^2}\right)\right]$$

C: Concentration [g/m³] | Q: Emission Rate [g/s] | u: Wind Speed [m/s] | He: Effective Stack Height (physical height + plume rise) [m] | σy, σz: Horizontal & Vertical Dispersion Coefficients [m], which are functions of downwind distance x and the Atmospheric Stability Class.

The effective stack height He is often more important than the physical height. It's calculated using Briggs plume rise formulas, which balance the initial momentum and buoyancy of the stack gas against the ambient wind and stability.

$$\Delta h = \frac{1.6 F_b^{1/3}x^{2/3}}{u}\quad \text{(for buoyancy-dominated plumes)}$$

Δh: Plume Rise [m] | Fb: Buoyancy Flux [m⁴/s³] | x: Downwind Distance [m]. The buoyancy flux depends on the temperature difference (Ts - Ta) and stack diameter. This is why tweaking the gas temperature in the simulator has such a dramatic effect.

Frequently Asked Questions

Atmospheric stability is classified from A (strongly unstable) to F (stable) based on wind speed, solar radiation (daytime), and cloud cover (nighttime). In this tool, it can be easily selected from a dropdown menu. Since unstable conditions lead to faster dispersion and stable conditions allow high concentrations to travel farther, choose the appropriate class according to your evaluation purpose.
Ground-level concentrations (z=0) are calculated at each downwind point along the wind direction, and the maximum value and its location are automatically extracted. The maximum concentration is proportional to the emission rate Q and inversely proportional to the wind speed u. The more stable the condition (e.g., F), the higher the maximum concentration and the longer the downwind distance tends to be.
This model assumes flat terrain. Turbulence and downwash effects caused by buildings are not considered. In practice, the stack height should be at least 2.5 times the building height, or a separate building wake correction (e.g., EPA method) should be applied.
The main causes are: (1) an excessively high emission rate Q, (2) an extremely low wind speed u (e.g., less than 1 m/s), or (3) stable class F conditions with near-calm winds. The Gaussian plume model is not applicable under low wind or calm conditions. It is recommended to use wind speeds of 1 m/s or higher.

Real-World Applications

Environmental Impact Assessments (EIA): Before building a new power plant or factory, engineers use this model to predict ground-level pollutant concentrations. They test different stack heights and emission rates to ensure compliance with air quality standards, like the WHO guideline of 5 μg/m³ for annual PM2.5.

Emergency Response Planning: For accidental releases of hazardous gases from industrial facilities, Gaussian models provide a first, rapid estimate of the affected area and concentration levels, helping to plan evacuation zones and emergency protocols.

Regulatory Permit Applications: Companies must apply for permits to operate emission sources. Regulatory bodies (like the US EPA) often accept screening-level analyses using Gaussian plume models like AERMOD, which is based on these principles, to grant or deny permits.

Pre-Check for Detailed CFD Simulations: In CAE workflows, this simple model is a crucial first step. An engineer might run this simulator to identify worst-case scenarios (e.g., low wind speed, stable atmosphere) before launching a computationally expensive 3D CFD simulation in OpenFOAM or ANSYS Fluent for a more detailed, site-specific analysis.

Common Misconceptions and Points to Note

While this simulator is powerful, using it incorrectly carries the risk of trusting results that are far removed from reality. The first key point to grasp is that "the Gaussian plume model deals with time-averaged steady states." This means it cannot reproduce instantaneous puffs of smoke or situations where wind direction changes frequently. For example, phenomena like "downdrafts" near an emission source causing smoke to be driven into the ground are often not fully captured by this basic model.

Next, beware of pitfalls in parameter settings. The "effective stack height" is particularly crucial. While the simulator automatically calculates the buoyancy rise, in real-world design, the influence of terrain (hills, buildings) is enormous. Even if a calculation for flat ground shows "no problem," if there is a building downwind, the "building wake effect" can occur, creating vortices behind it and causing unexpectedly high concentrations. Before entering parameters, develop the habit of visualizing the surrounding terrain and the wind's path.

Finally, avoid focusing solely on the "maximum ground-level concentration" number. It is certainly an important metric, but environmental standards often require statistical evaluations, such as "the 98th percentile of 1-hour values." What you obtain from this tool is merely the concentration distribution under specific conditions. In practice, methods like the "Sintal method," which combines annual meteorological data (frequency distributions of wind direction, speed, and stability) to evaluate long-term average concentrations, are used. It's wise to view the tool's results as a "first-step screening."