INGENIA

ENV-06

Gaussian plume (ground axis)

C = Q /(π u σy σz) exp(−H² /(2 σz²)) at y = 0.

Reading speed
Air qualityPasquill–GiffordEPA

Governing equation

C=Qπuσyσzexp ⁣(H22σz2)C=\dfrac{Q}{\pi u\sigma_y\sigma_z}\exp\!\left(-\dfrac{H^2}{2\sigma_z^2}\right)

where

Q
Emission rate (g/s)
u
Wind speed (m/s)
\sigma_y
Lateral σ (m)
\sigma_z
Vertical σ (m)
H
Effective height (m)
C
Centreline concentration (mg/m³)

Lecture brief

Historical brief

Streeter–Phelps (1925) oxygen sag, settling theory and Guldberg–Waage kinetics made water and air quality a rate problem. The lab computes sag, overflow and a snapshot of reactor mass balance. This sheet (ENV-06 — Gaussian plume (ground axis)) is the form associated with Pasquill–Gifford · EPA. Working symbols: QQ, uu, σy\sigma_y, σz\sigma_z, HH \rightarrow CC. The steady advection–diffusion equation with constant wind and Gaussian closures is the Gaussian plume, still the regulatory workhorse.

Purpose

Purpose: compute CC from QQ, uu, σy\sigma_y, σz\sigma_z, HH in Environmental via C=Qπuσyσzexp ⁣(H22σz2)C=\dfrac{Q}{\pi u\sigma_y\sigma_z}\exp\!\left(-\dfrac{H^2}{2\sigma_z^2}\right) C = Q /(π u σy σz) exp(−H² /(2 σz²)) at y = 0. Use it when a real environmental question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given Q=10.000g/sQ = 10.000\,\mathrm{g/s}, u=4.000m/su = 4.000\,\mathrm{m/s}, σy=80.000m\sigma_y = 80.000\,\mathrm{m}, σz=30.000m\sigma_z = 30.000\,\mathrm{m}, H=50.000mH = 50.000\,\mathrm{m}, the governing relation C=Qπuσyσzexp ⁣(H22σz2)C=\dfrac{Q}{\pi u\sigma_y\sigma_z}\exp\!\left(-\dfrac{H^2}{2\sigma_z^2}\right) yields C=0.0827mg/m3C = 0.0827\,\mathrm{mg/m^{3}}. Ground-level centreline, total reflection, enter σy, σz. Move a slider: the numbers are this situation, not a canned story.

Calculator

Inputs

Outputs

  • Centreline concentration C0.0827 mg/m³
Reading speed

Watch on YouTube

Free library

Full library

Free PDF / open book

YouTube channels

ENV-06 · curve
00:0 / 00:08

Narration of this film

Ground-level centreline, total reflection, enter σy, σz.

The steady advection–diffusion equation with constant wind and Gaussian closures is the Gaussian plume, still the regulatory workhorse.

Reading speed

Watch on YouTube