study guide

Babygirl90
handout2.pdf

EHST 3600: Air Pollution 1

LAST SESSION REVIEW

• Wind velocity profile

• Planetary boundary layer

• Gradient wind

• Maximum mixing depth

• Rawinsonde measurements

• Horizontal dispersion of pollutants

• Wind speed and direction

• Wind rose

• Atmospheric turbulence

• Thermal

• Mechanical

• Stack plume characteristics

• Looping

• Coning

• Fanning

• Fumigation

• Lofting

• Trapping

• Plume behavior

• Terrain

• Buildings

LAST SESSION REVIEW

• Urban heat island effect

• Human impact on earth-atmosphere system

• Depletion of the ozone layer

• Health and ecological effects

• Rising levels of atmospheric CO2

DISPERSION OF POLLUTANTS IN THE ATMOSPHERE

EHST 3600: Air Pollution

SESSION OBJECTIVES

• To know the dispersion of pollutants

• To know the factors affecting dispersion of pollutants

• To know micro- and macro-scale dispersion of pollutants

• To know how to calculate effective stack height

SESSION OUTLINE

• Settling velocity

• The eddy diffusion model

• The Gaussian dispersion model

• Calculation of the effective stack height

ATMOSPHERIC DISPERSION OF EFFLUENTS FROM SOURCES

• Physical and chemical nature of effluents

• Meteorological characteristics of the environment

• Location of the stack with relation to obstructions to air motion

• Nature of the terrain downwind from the stack

EHST 3600: Air Pollution 2

SETTLING VELOCITY • Low settling velocity

• Gases

• Fine particles (20 um or smaller)

• Larger settling velocity

• Large particles • Results in a higher

ground-level concentration of

the solid pollutant closer to the stack than is the case for gases.

• No wind speed • Low-density plumes tend to

reach high elevations; ground

concentrations are low • Large particles and dense gas

plumes fall to the ground in the vicinity of the stack

• High wind speed

• Increases the diluting action of the atmosphere

• Gives rise to lower ground- level concentrations downwind from the stack

𝑉𝑠 𝑢 ≥ 1.5

PREVENTION OF DOWNWASH

To achieve maximum

dispersion, the

effluents should leave the stack with

sufficient momentum and

buoyancy that they

continue to rise from the stack exit.

𝑉𝑠 𝑢 ≥ 1.5

• Stack gas velocity (Vs) = 6.8 mph

• Wind velocity on top of stack (u) = 6.0 mph

• Possibility of downwash?

• If <1.5, calculate the reduced stack height:

ℎ𝑠 ′ = ℎ𝑠 + 2𝑑𝑠

𝑉𝑠 𝑢𝑠 − 1.5

hs

THE EDDY DIFFUSION MODEL

• Any diffusion process by which

substances are mixed in the

atmosphere or in any fluid system due

to eddy motion

• Involves the use of the “mixing length”

concept

• Basis of the most comprehensive approach to transport theory

• Usual starting point in the development of a dispersion model for the atmosphere

GAUSSIAN DISPERSION MODEL

Fig. 4-2

H = effective stack height

hs = stack height

h = plume rise

• Stack characteristics

• Meteorological

conditions

• Physical and chemical

nature of the effluent

H = hs + h

CALCULATION OF THE EFFECTIVE STACK HEIGHT

• Determine if there is downwash of plume due to low exit velocity

• 𝑉𝑠

𝑢 ≥ 1.5  downwash is negligible  ℎ𝑠

′ = ℎ𝑠

• 𝑉𝑠

𝑢 < 1.5  downwash is likely  calculate the reduced stack height, ℎ𝑠

′ :

• ℎ𝑠 ′ = ℎ𝑠 + 2𝑑𝑠

𝑉𝑠

𝑢𝑠 − 1.5

𝑉𝑠 - stack velocity (m/s) 𝑢 – wind speed measured at the height, ℎ𝑠 ℎ𝑠 - physical stack height (m) 𝑑𝑠 - stack exit diameter (m)

CALCULATION OF THE EFFECTIVE STACK HEIGHT

• Determine stability category:

• Unstable or neutral condition

• Stable condition

• Calculate the buoyancy flux, 𝐹𝑏

• 𝐹𝑏 = 𝑔𝑉𝑠𝑑𝑠 2 𝑇𝑠−𝑇𝑎

4𝑇𝑠  < or  55 m4/s3 where g = 9.8 m/s2

• Calculate the crossover temperature difference, (T)c

• Calculate the difference between the stack gas and ambient temp, T

• ∆𝑇 = 𝑇𝑠 − 𝑇𝑎

EHST 3600: Air Pollution 3

CALCULATION OF THE EFFECTIVE STACK HEIGHT

• Compare (T)c and T to determine where plume rise is dominated by momentum or buoyancy

H = hs + h

PROBLEM SOLVING

Example 4-6

• Wind speed at top of stack = 3 m/s

• Stack gas velocity = 6 m/s

• Stack diameter = 2 m

• Physical stack height = 40 m

• Atmospheric stability = neutral

• Air temp = 300 K

• Stack temp = 440 K

SUMMARY

• Settling velocity

• The eddy diffusion model

• The Gaussian dispersion model

• Calculation of the effective stack height

• Plume downwash

• Atmosphere stability conditions

• Buoyancy flux, Fb

• Crossover temperature difference, (T)c

• Difference between the stack gas and ambient temp, T

• Plume rise, h