Skip to content

Atmospheric Dispersion Modeling (Gaussian)

Environmental Engineering · FE Reference Handbook section

Environmental Engineering
15 formulas
10 exam-style examples
~60 min
All Environmental Engineering lectures

Handbook notes for this section

Definitions and conditions exactly as the handbook states them.

  • Maximum concentration at ground level and directly downwind from an elevated source.
  • where variables are as above except

Core formulas for this FE topic

Definitions, applicability, units, assumptions and worked examples for each relation.

Worked exam-style examples

The four ways this section is written on the real exam — thoughts first, then equations, then substitution.

Example 1
Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration — Atmospheric Dispersion Modeling (Gaussian)

atmospheric dispersion modeling of a Gaussian plume from a power plant stack Given emission rate (Q) = 97.0000 g/s; wind speed (u) = 6.2000 m/s; horizontal dispersion coeff (sigma_y) = 73.0000 m; vertical dispersion coeff (sigma_z) = 29.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m, determine the centerline ground concentration (C) in g/m^3.

Given

  • emissionrate(Q)=97.0000g/semission rate (Q) = 97.0000 g/s
  • windspeed(u)=6.2000m/swind speed (u) = 6.2000 m/s
  • horizontaldispersioncoeff(sigmay)=73.0000mhorizontal dispersion coeff (sigma_y) = 73.0000 m
  • verticaldispersioncoeff(sigmaz)=29.0000mvertical dispersion coeff (sigma_z) = 29.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m

Find

centerline ground concentration (C), in g/m^3

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except C is given, so isolate C symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 1 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration — Atmospheric Dispersion Modeling (Gaussian)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for C:

    C=Q2πuσyσzC = \dfrac{Q}{2\pi u \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 97.0000 g/s, wind speed (u) = 6.2000 m/s, horizontal dispersion coeff (sigma_y) = 73.0000 m, vertical dispersion coeff (sigma_z) = 29.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m.

  4. Step 4 — Substitute the given values:

    C=97.00002π6.2000σ0.0000σzC = \dfrac{97.0000}{2\pi 6.2000 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    C = 0.0012\ \text{g/m^3}
  6. Step 6 — Check: returning C = 0.0012 g/m^3 to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
C = 0.0012\ \text{g/m^3}

Why the other options are there

  • 0.0024 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0006 — dropped that same factor in the other direction.
  • 0.0013 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 2
Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate — Atmospheric Dispersion Modeling (Gaussian) (2)

Gaussian dispersion model for a chemical plant emission source Given wind speed (u) = 9.6000 m/s; horizontal dispersion coeff (sigma_y) = 299.0 m; vertical dispersion coeff (sigma_z) = 115.0 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.9293 g/m^3, determine the emission rate (Q) in g/s.

Given

  • windspeed(u)=9.6000m/swind speed (u) = 9.6000 m/s
  • horizontaldispersioncoeff(sigmay)=299.0mhorizontal dispersion coeff (sigma_y) = 299.0 m
  • verticaldispersioncoeff(sigmaz)=115.0mvertical dispersion coeff (sigma_z) = 115.0 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.9293g/m3centerline ground concentration (C) = 0.9293 g/m^3

Find

emission rate (Q), in g/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except Q is given, so isolate Q symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 2 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate — Atmospheric Dispersion Modeling (Gaussian) (2)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for Q:

    Q=C 2πuσyσzQ = C\,2\pi u \sigma_y \sigma_z
  3. Step 3 — List the givens: wind speed (u) = 9.6000 m/s, horizontal dispersion coeff (sigma_y) = 299.0 m, vertical dispersion coeff (sigma_z) = 115.0 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.9293 g/m^3.

  4. Step 4 — Substitute the given values:

    Q=0.9293 2π9.6000σ0.0000σzQ = 0.9293\,2\pi 9.6000 \sigma_0.0000 \sigma_z
  5. Step 5 — Evaluate:

    Q=1927506 g/sQ = 1927506\ \text{g/s}
  6. Step 6 — Check: returning Q = 1,927,506 g/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
Q=1927506 g/sQ = 1927506\ \text{g/s}

Why the other options are there

  • 3,855,012 — kept a factor of two that cancels in the correct rearrangement.
  • 963,753 — dropped that same factor in the other direction.
  • 2,120,256 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 3
Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed — Atmospheric Dispersion Modeling (Gaussian) (3)

atmospheric dispersion Gaussian plume centerline concentration downwind Given emission rate (Q) = 80.0000 g/s; horizontal dispersion coeff (sigma_y) = 98.0000 m; vertical dispersion coeff (sigma_z) = 85.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.9756 g/m^3, determine the wind speed (u) in m/s.

Given

  • emissionrate(Q)=80.0000g/semission rate (Q) = 80.0000 g/s
  • horizontaldispersioncoeff(sigmay)=98.0000mhorizontal dispersion coeff (sigma_y) = 98.0000 m
  • verticaldispersioncoeff(sigmaz)=85.0000mvertical dispersion coeff (sigma_z) = 85.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.9756g/m3centerline ground concentration (C) = 0.9756 g/m^3

Find

wind speed (u), in m/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except u is given, so isolate u symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 3 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed — Atmospheric Dispersion Modeling (Gaussian) (3)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for u:

    u=Q2πCσyσzu = \dfrac{Q}{2\pi C \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 80.0000 g/s, horizontal dispersion coeff (sigma_y) = 98.0000 m, vertical dispersion coeff (sigma_z) = 85.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.9756 g/m^3.

  4. Step 4 — Substitute the given values:

    u=80.00002π0.9756σ0.0000σzu = \dfrac{80.0000}{2\pi 0.9756 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    u=0.0016 m/su = 0.0016\ \text{m/s}
  6. Step 6 — Check: returning u = 0.0016 m/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
u=0.0016 m/su = 0.0016\ \text{m/s}

Why the other options are there

  • 0.0031 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0008 — dropped that same factor in the other direction.
  • 0.0017 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 4
Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 2) — Atmospheric Dispersion Modeling (Gaussian) (4)

atmospheric dispersion modeling of a Gaussian plume from a power plant stack Given emission rate (Q) = 78.0000 g/s; wind speed (u) = 8.6000 m/s; horizontal dispersion coeff (sigma_y) = 238.0 m; vertical dispersion coeff (sigma_z) = 43.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m, determine the centerline ground concentration (C) in g/m^3.

Given

  • emissionrate(Q)=78.0000g/semission rate (Q) = 78.0000 g/s
  • windspeed(u)=8.6000m/swind speed (u) = 8.6000 m/s
  • horizontaldispersioncoeff(sigmay)=238.0mhorizontal dispersion coeff (sigma_y) = 238.0 m
  • verticaldispersioncoeff(sigmaz)=43.0000mvertical dispersion coeff (sigma_z) = 43.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m

Find

centerline ground concentration (C), in g/m^3

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except C is given, so isolate C symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 4 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 2) — Atmospheric Dispersion Modeling (Gaussian) (4)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for C:

    C=Q2πuσyσzC = \dfrac{Q}{2\pi u \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 78.0000 g/s, wind speed (u) = 8.6000 m/s, horizontal dispersion coeff (sigma_y) = 238.0 m, vertical dispersion coeff (sigma_z) = 43.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m.

  4. Step 4 — Substitute the given values:

    C=78.00002π8.6000σ0.0000σzC = \dfrac{78.0000}{2\pi 8.6000 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    C = 0.0001\ \text{g/m^3}
  6. Step 6 — Check: returning C = 0.0001 g/m^3 to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
C = 0.0001\ \text{g/m^3}

Why the other options are there

  • 0.0003 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0001 — dropped that same factor in the other direction.
  • 0.0002 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 5
Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate (case 2) — Atmospheric Dispersion Modeling (Gaussian) (5)

Gaussian dispersion model for a chemical plant emission source Given wind speed (u) = 4.6000 m/s; horizontal dispersion coeff (sigma_y) = 61.0000 m; vertical dispersion coeff (sigma_z) = 39.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.1419 g/m^3, determine the emission rate (Q) in g/s.

Given

  • windspeed(u)=4.6000m/swind speed (u) = 4.6000 m/s
  • horizontaldispersioncoeff(sigmay)=61.0000mhorizontal dispersion coeff (sigma_y) = 61.0000 m
  • verticaldispersioncoeff(sigmaz)=39.0000mvertical dispersion coeff (sigma_z) = 39.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.1419g/m3centerline ground concentration (C) = 0.1419 g/m^3

Find

emission rate (Q), in g/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except Q is given, so isolate Q symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 5 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate (case 2) — Atmospheric Dispersion Modeling (Gaussian) (5)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for Q:

    Q=C 2πuσyσzQ = C\,2\pi u \sigma_y \sigma_z
  3. Step 3 — List the givens: wind speed (u) = 4.6000 m/s, horizontal dispersion coeff (sigma_y) = 61.0000 m, vertical dispersion coeff (sigma_z) = 39.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.1419 g/m^3.

  4. Step 4 — Substitute the given values:

    Q=0.1419 2π4.6000σ0.0000σzQ = 0.1419\,2\pi 4.6000 \sigma_0.0000 \sigma_z
  5. Step 5 — Evaluate:

    Q=9758 g/sQ = 9758\ \text{g/s}
  6. Step 6 — Check: returning Q = 9,758 g/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
Q=9758 g/sQ = 9758\ \text{g/s}

Why the other options are there

  • 19,515 — kept a factor of two that cancels in the correct rearrangement.
  • 4,879 — dropped that same factor in the other direction.
  • 10,733 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 6
Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed (case 2) — Atmospheric Dispersion Modeling (Gaussian) (6)

atmospheric dispersion Gaussian plume centerline concentration downwind Given emission rate (Q) = 175.0 g/s; horizontal dispersion coeff (sigma_y) = 50.0000 m; vertical dispersion coeff (sigma_z) = 49.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.9013 g/m^3, determine the wind speed (u) in m/s.

Given

  • emissionrate(Q)=175.0g/semission rate (Q) = 175.0 g/s
  • horizontaldispersioncoeff(sigmay)=50.0000mhorizontal dispersion coeff (sigma_y) = 50.0000 m
  • verticaldispersioncoeff(sigmaz)=49.0000mvertical dispersion coeff (sigma_z) = 49.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.9013g/m3centerline ground concentration (C) = 0.9013 g/m^3

Find

wind speed (u), in m/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except u is given, so isolate u symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 6 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed (case 2) — Atmospheric Dispersion Modeling (Gaussian) (6)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for u:

    u=Q2πCσyσzu = \dfrac{Q}{2\pi C \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 175.0 g/s, horizontal dispersion coeff (sigma_y) = 50.0000 m, vertical dispersion coeff (sigma_z) = 49.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.9013 g/m^3.

  4. Step 4 — Substitute the given values:

    u=175.02π0.9013σ0.0000σzu = \dfrac{175.0}{2\pi 0.9013 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    u=0.0126 m/su = 0.0126\ \text{m/s}
  6. Step 6 — Check: returning u = 0.0126 m/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
u=0.0126 m/su = 0.0126\ \text{m/s}

Why the other options are there

  • 0.0252 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0063 — dropped that same factor in the other direction.
  • 0.0139 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 7
Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 3) — Atmospheric Dispersion Modeling (Gaussian) (7)

atmospheric dispersion modeling of a Gaussian plume from a power plant stack Given emission rate (Q) = 57.0000 g/s; wind speed (u) = 8.6000 m/s; horizontal dispersion coeff (sigma_y) = 93.0000 m; vertical dispersion coeff (sigma_z) = 103.0 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m, determine the centerline ground concentration (C) in g/m^3.

Given

  • emissionrate(Q)=57.0000g/semission rate (Q) = 57.0000 g/s
  • windspeed(u)=8.6000m/swind speed (u) = 8.6000 m/s
  • horizontaldispersioncoeff(sigmay)=93.0000mhorizontal dispersion coeff (sigma_y) = 93.0000 m
  • verticaldispersioncoeff(sigmaz)=103.0mvertical dispersion coeff (sigma_z) = 103.0 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m

Find

centerline ground concentration (C), in g/m^3

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except C is given, so isolate C symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 7 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 3) — Atmospheric Dispersion Modeling (Gaussian) (7)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for C:

    C=Q2πuσyσzC = \dfrac{Q}{2\pi u \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 57.0000 g/s, wind speed (u) = 8.6000 m/s, horizontal dispersion coeff (sigma_y) = 93.0000 m, vertical dispersion coeff (sigma_z) = 103.0 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m.

  4. Step 4 — Substitute the given values:

    C=57.00002π8.6000σ0.0000σzC = \dfrac{57.0000}{2\pi 8.6000 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    C = 0.0001\ \text{g/m^3}
  6. Step 6 — Check: returning C = 0.0001 g/m^3 to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
C = 0.0001\ \text{g/m^3}

Why the other options are there

  • 0.0002 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0001 — dropped that same factor in the other direction.
  • 0.0001 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 8
Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate (case 3) — Atmospheric Dispersion Modeling (Gaussian) (8)

Gaussian dispersion model for a chemical plant emission source Given wind speed (u) = 4.1000 m/s; horizontal dispersion coeff (sigma_y) = 41.0000 m; vertical dispersion coeff (sigma_z) = 23.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.4548 g/m^3, determine the emission rate (Q) in g/s.

Given

  • windspeed(u)=4.1000m/swind speed (u) = 4.1000 m/s
  • horizontaldispersioncoeff(sigmay)=41.0000mhorizontal dispersion coeff (sigma_y) = 41.0000 m
  • verticaldispersioncoeff(sigmaz)=23.0000mvertical dispersion coeff (sigma_z) = 23.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.4548g/m3centerline ground concentration (C) = 0.4548 g/m^3

Find

emission rate (Q), in g/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except Q is given, so isolate Q symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 8 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for emission rate (case 3) — Atmospheric Dispersion Modeling (Gaussian) (8)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for Q:

    Q=C 2πuσyσzQ = C\,2\pi u \sigma_y \sigma_z
  3. Step 3 — List the givens: wind speed (u) = 4.1000 m/s, horizontal dispersion coeff (sigma_y) = 41.0000 m, vertical dispersion coeff (sigma_z) = 23.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.4548 g/m^3.

  4. Step 4 — Substitute the given values:

    Q=0.4548 2π4.1000σ0.0000σzQ = 0.4548\,2\pi 4.1000 \sigma_0.0000 \sigma_z
  5. Step 5 — Evaluate:

    Q=11049 g/sQ = 11049\ \text{g/s}
  6. Step 6 — Check: returning Q = 11,049 g/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
Q=11049 g/sQ = 11049\ \text{g/s}

Why the other options are there

  • 22,098 — kept a factor of two that cancels in the correct rearrangement.
  • 5,525 — dropped that same factor in the other direction.
  • 12,154 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 9
Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed (case 3) — Atmospheric Dispersion Modeling (Gaussian) (9)

atmospheric dispersion Gaussian plume centerline concentration downwind Given emission rate (Q) = 31.0000 g/s; horizontal dispersion coeff (sigma_y) = 212.0 m; vertical dispersion coeff (sigma_z) = 132.0 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m; centerline ground concentration (C) = 0.6298 g/m^3, determine the wind speed (u) in m/s.

Given

  • emissionrate(Q)=31.0000g/semission rate (Q) = 31.0000 g/s
  • horizontaldispersioncoeff(sigmay)=212.0mhorizontal dispersion coeff (sigma_y) = 212.0 m
  • verticaldispersioncoeff(sigmaz)=132.0mvertical dispersion coeff (sigma_z) = 132.0 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m
  • centerlinegroundconcentration(C)=0.6298g/m3centerline ground concentration (C) = 0.6298 g/m^3

Find

wind speed (u), in m/s

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except u is given, so isolate u symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 9 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for wind speed (case 3) — Atmospheric Dispersion Modeling (Gaussian) (9)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for u:

    u=Q2πCσyσzu = \dfrac{Q}{2\pi C \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 31.0000 g/s, horizontal dispersion coeff (sigma_y) = 212.0 m, vertical dispersion coeff (sigma_z) = 132.0 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m, centerline ground concentration (C) = 0.6298 g/m^3.

  4. Step 4 — Substitute the given values:

    u=31.00002π0.6298σ0.0000σzu = \dfrac{31.0000}{2\pi 0.6298 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    u=0.0003 m/su = 0.0003\ \text{m/s}
  6. Step 6 — Check: returning u = 0.0003 m/s to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
u=0.0003 m/su = 0.0003\ \text{m/s}

Why the other options are there

  • 0.0006 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0001 — dropped that same factor in the other direction.
  • 0.0003 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

Example 10
Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 4) — Atmospheric Dispersion Modeling (Gaussian) (10)

atmospheric dispersion modeling of a Gaussian plume from a power plant stack Given emission rate (Q) = 192.0 g/s; wind speed (u) = 5.5000 m/s; horizontal dispersion coeff (sigma_y) = 28.0000 m; vertical dispersion coeff (sigma_z) = 47.0000 m; crosswind distance (y) = 0.0000 m; effective stack height (H) = 0.0000 m, determine the centerline ground concentration (C) in g/m^3.

Given

  • emissionrate(Q)=192.0g/semission rate (Q) = 192.0 g/s
  • windspeed(u)=5.5000m/swind speed (u) = 5.5000 m/s
  • horizontaldispersioncoeff(sigmay)=28.0000mhorizontal dispersion coeff (sigma_y) = 28.0000 m
  • verticaldispersioncoeff(sigmaz)=47.0000mvertical dispersion coeff (sigma_z) = 47.0000 m
  • crosswinddistance(y)=0.0000mcrosswind distance (y) = 0.0000 m
  • effectivestackheight(H)=0.0000meffective stack height (H) = 0.0000 m

Find

centerline ground concentration (C), in g/m^3

Start with the thinking

  • The governing relation printed in this handbook section is Atmospheric Dispersion Modeling (Gaussian).
  • Everything except C is given, so isolate C symbolically first — never rearrange after the numbers are in.
  • Tabulate each given with its unit and confirm the units are consistent with the relation before substituting.
  • Atmospheric dispersion modeling with the Gaussian plume equation estimates ground-level concentration downwind of a stack.
downwind distanceconcentrationGaussian dispersion plume centerline

Figure 10 — schematic for Atmospheric Dispersion Modeling (Gaussian) — solve for centerline ground concentration (case 4) — Atmospheric Dispersion Modeling (Gaussian) (10)

Step-by-step solution

  1. Step 1 — State the governing relation:

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}
  2. Step 2 — Rearrange symbolically for C:

    C=Q2πuσyσzC = \dfrac{Q}{2\pi u \sigma_y \sigma_z}
  3. Step 3 — List the givens: emission rate (Q) = 192.0 g/s, wind speed (u) = 5.5000 m/s, horizontal dispersion coeff (sigma_y) = 28.0000 m, vertical dispersion coeff (sigma_z) = 47.0000 m, crosswind distance (y) = 0.0000 m, effective stack height (H) = 0.0000 m.

  4. Step 4 — Substitute the given values:

    C=192.02π5.5000σ0.0000σzC = \dfrac{192.0}{2\pi 5.5000 \sigma_0.0000 \sigma_z}
  5. Step 5 — Evaluate:

    C = 0.0042\ \text{g/m^3}
  6. Step 6 — Check: returning C = 0.0042 g/m^3 to

    C=Q2πuσyσze−y22σy2e−H22σz2C = \dfrac{Q}{2\pi u \sigma_y \sigma_z} e^{-\frac{y^2}{2\sigma_y^2}} e^{-\frac{H^2}{2\sigma_z^2}}

    reproduces the given quantities, and both sides carry the same units.

Answer:
C = 0.0042\ \text{g/m^3}

Why the other options are there

  • 0.0084 — kept a factor of two that cancels in the correct rearrangement.
  • 0.0021 — dropped that same factor in the other direction.
  • 0.0046 — rounded an intermediate value before the final step.

Reference: FE Handbook — Atmospheric Dispersion Modeling

© 2026 Dr. Steve Efe. Civil Engineering Capstone Studio. All rights reserved.