Emitting Education
by Anthony J. Sadar CCM
January 1, 2009
A simply constructed, artificial smokestack safely demonstrates the dispersion of toxic air pollutants.
Learning the concepts of air pollution
dispersion for the first time can be quite challenging. Even if the qualitative
portions of the topic are not so hard to grasp, the quantitative, formulaic
parts can be downright intimidating. One method educators and trainers can use
to break through such barriers is a physical modeling tool, labeled The SuperStack
by the author, which realistically and safely demonstrates the dispersion of
atmospheric contaminants using paper hole-punches to represent pollution
particles. The artificial stack is 13 feet tall with a uniform 4-inch inside
diameter, but can be used to provide practical, hands-on experience for stacks
of a much grander scale.
Modeling theory
Before explaining how this practical equipment can be used
to teach the fundamentals of air-pollution dispersion, it is important to
understand basic dispersion modeling theory.
The three primary components of the air pollution
system (elaborated on later) are emission sources, the atmosphere
and receptors of contaminants. The unifying formula for the
relationship among these components is:
Where:
C = concentration (g/m 3), the impact
of the source(s) on the receptor(s)
Q = emission rate (g/s), the contaminant quantity/time
release into the atmosphere
S = stability (m-2), a critical weather condition related to
the air’s mixing potential
U = wind speed (m/s), critical weather condition related to
downwind transport of contaminants.
Scientists and engineers who study air pollution
dispersion will frequently rely on a basic Gaussian plume equation, derived
from empirical studies and statistical analysis, e.g. probability density
function, to quantitatively estimate the concentration of atmospheric
contaminants downwind of an emission source. A simplified version of the
Gaussian plume equation follows:
Where:
Xi = contaminant concentration in the atmosphere (g/m3) at
a specified downwind distance
q = uniform, continuous emission rate (g/s)
pi
= 3.1416
mu
= average wind speed (m/s) in the atmosphere downwind of the source
sigmay
= cross-wind dispersion parameter (m) at a specified downwind distance
sigmaz
= vertical dispersion parameter (m) at a specified downwind distance
H = emission height (m).
(Note that “exp ” is typically designated as “ex
” on calculators. Also note that in the equations and text that that follow, m
= meters, m2 = meters squared (area), m3
= meters cubed (volume), g = grams, mg/m3 = micrograms per cubic
meter, and s = seconds.)
Basically, such equations are developed to approximate
a downwind concentration (mass of a contaminant in a volume of air, typically
in g/m3), given a known or
estimated air release rate (contaminant loading per second, g/s), airflow (wind
speed in distance per second, m/s) and atmospheric stability conditions across
the impact area (in m2). As such, any formula that can simulate
emission dispersal under specified weather and topographic conditions can be a
valuable tool to an air quality scientist, engineer or emergency response
personnel.
Modeling instruction and demonstration
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| A – Figure 1 shows the stack assembly with wooden base and support structure, along with a portable, two-speed blower motor coupled to the base of the stack. The stack is 13-feet tall with an I.D. of 4 inches. It can be separated to simulate shorter stack heights, while a two-speed blower can alter exit-gas velocities. |
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The stack simulator can be used to help students more fully
comprehend the real world significance of the basic Gaussian plume equation.
Furthermore, combining a physical model with a computational model such as the
Gaussian plume equation can strengthen conceptual and quantitative
understanding of the complex reality of chemical dispersion in air.
To combine these two models for more effective
teaching/training, first, the instructor must introduce the general ideas of
contaminant dispersion using the unifying formula presented above. Examples of
sources and receptors, and key atmospheric dispersion components can be
elicited from students. Alternatively, prior to revealing the unifying formula,
students can be encouraged to construct a formula that represents the likely
relationship among the three parts of the air pollution system.
To
have students construct a formula, assign three variables to represent each
system component, e.g., S (source strength), D (dispersion from wind and
stability), and R (concentration at receptor). If necessary, students may be
prompted by being reminded to consider the units of each variable. R = S / D is
an appropriate solution.
Once the importance of the unifying formula, along with the
relationships among its variables, has been thoroughly explored, the instructor
can move on to introduce the basic Gaussian plume equation, and then compare
and contrast the formula with the plume equation. For instance, note that the
primary similarity between the formula and the equation is
that both use “q” in the numerator to represent emission rate in g/s and “u” in
the denominator to represent wind speed in m/s. (The difference here of course
is between capitalization/non-capitalization of the variables.)
One primary substantive difference
between the formula and the equation is that the “S” stability term in the
numerator of the formula is replaced by “pi, sigma y, sigma z”
in the denominator of the plume equation. Another primary difference is the
introduction of the expression “exp (- H2 / 2 sigma z2 )” to account for additional
dispersion of emissions released from an elevated source such as a smokestack.
(The complete explanation of the importance of these differences is beyond the
scope of this article, however, the similarity of the units of both sets of
terms along with statistical theory can be employed to elaborate on the
differences between the formula and equation.)
When students have grasped the crucial features of the
formulaic models of air dispersion, instructors can then introduce the
artificial stack and its real life application to the numerical models.
Now for the stack
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| Figure 2. The SuperStack is shown on the Geneva College campus with optional La Crosse Technology wind equipment (near stack top) and 1 m2 foam board for identifying particle concentrations downwind of the stack. |
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To begin, the source (smokestack)
features can be examined. A hole punch is used to make multi-colored paper
particles (the punched disks) that are inserted at the base of stack model. The
known amount of “particulate loading” versus the time over which the particles
are emitted out the stack provides the emission rate of the source, i.e., the
particles-per-second rate. If students measure the mean mass of each paper
particle, they can then determine the mass per second emission rate of
particles exiting the stack.
Additional stack parameters essential to computing downwind
particle emission impact should be identified and then measured. These
parameters include stack height and diameter, and exhaust temperature and velocity.
The artificial stack stands 13 feet high from its base to
its 4-inch exhaust opening. The stack can be separated to produce a 6.5-foot
unit. The present unit consists of a two-speed blower for low- and high-speed
flows that can be measured with, for example, a pitot tube anemometer through
the stack’s sampling port. Using a simple liquid-in-glass thermometer, the
stack gas temperature also can be measured through the port.
Atmospheric conditions such as wind speed and stability are
key to air dispersion and can be identified via visual observations (like the
Beaufort Scale for wind speed and cloud cover for stability estimates). Or
better, a meteorological tower that extends anemometer
equipment to the stack top can be constructed so that students can measure wind
direction and speed (see Figure 2). Experience has shown
that an approximately 15-mph sustained wind is needed to properly disperse the
particles emitted from the stack. (Note that precipitation is usually not
desirable during students’ first demonstrations, since paper particles will be
washed out of the air. However, precipitation can show the real world effects
of rain and heavy snowfall on particulate matter in subsequent sessions.)
Finally, the impact of the paper pollution particles on
downwind receptors can be demonstrated by counting the
portion of the total amount of particles that fall in a given area. To more
readily accomplish this task, a 1-m 2 foam board has been
fabricated (see Figure 2). One way in which this board can be used is to locate
the area of the highest concentration of particles on the ground, then
carefully lay the board over that area and trace out the board’s area using
chalk or string.
Once the board is removed, the number of particles per
square meter can be counted to yield the quantitative result of settled
particles per square meter. Furthermore, if it is assumed that these particles
represent all the particles that would also have impacted a 1-meter depth above
the 1-m 2 area in which they settled, then the number of
particles can now be equated to particles per cubic meter. Lastly, if the mean
mass of each paper particle has been measured, the students can then determine
the maximum mass per cubic meter concentration of particles that impacted the
environment downwind of the stack.
Conclusion
What has been included here identifies some of
the stack’s applications to assist students with their full comprehension of
the characteristics of contaminant dispersion, and the meaning (including
purpose, applicability and significance) of the air dispersion equations. PE Acknowledgement The author thanks Dr. James Gidley, Chair of the Engineering
Department at Geneva College, for suggesting the title Super Stack. The
author’s original title was Toxic Tower, which still may be used on occasion to
attract interest in the equipment.
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