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15318084 Anneke Sekar Sarinastiti Resume Inggris

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Final Project Seminar for Environmental Engineering Programme
Period of September 2022
Application and Performance Evaluation of CALPUFF dan AERMOD Modeling System
to Simulate TSP, SO2, AND NO2 Pollutant Dispersion : a Case Study at PT. X
Anneke Sekar Sarinastiti1 dan Dr. Asep Sofyan, S.T, M.T.2
Environmental Engineering Undergraduate Programme
Faculty of Civil and Environmental Engineering, Bandung Institute of Technology
St. Ganesha 10, Bandung, 40132
annekesekar@gmail.com; asepsofyan@gmail.com
ABSTRACT: Air pollution is the entry or inclusion of substances, energy, from other components into the ambient
air by human activities so that air quality decreases to a certain level. To protect an area from air pollution, it is
necessary to have a strategy to manage air quality, one of which is by predicting the dispersion of pollutants from
a source using a modeling application. study area, and accuracy of prediction results with actual concentrations in
ambient. In this study, two modeling applications were used, namely the Lagrangian-based CALPUFF model, nonsteady state, and the Gaussian Plume-based, steady state AERMOD model. This research was conducted in Central
Cikarang District, Bekasi Regency, with pollutant emission sources TSP, SO 2, and NO2 from the chimney of PT.
X. To determine the accuracy of the two models, several types of statistical tests are used, namely correlation
coefficient (R), Index of Agreement (IOA), Fractional Bias (FB), Root Mean Square Error (RMSE), Error, and
Mean Bias (MB). The results of this study indicate that the highest concentration for each pollutant and its location
has different values in CALPUFF and AERMOD. CALPUFF always yielded higher values in the highest predicted
concentrations (0.40359 µg/m3 for TSP, 0.60554 µg/m3 for SO2, and 0.43214 µg/m3 for NO2) than AERMOD
(0.04267 µg/m3 for TSP, 0.03646 µg/m3 for SO2, and 0.4516 µg/m3 for NO2). Overall, CALPUFF has a better
performance in modeling TSP, SO2, and NO2 pollutants than AERMOD as evidenced by statistical tests on the
results of the dispersion of the two models.
Keywords: AERMOD, air pollution, ambient, CALPUFF, concentration, dispersion, and modeling.
1.
INTRODUCTION
To protect an area from air pollution, it is necessary to have a strategy to manage air quality. The air
quality monitoring system is a strategy to determine the level of pollution in an area and an action plan
to implement policies and laws and regulations for air quality management. In this strategy, a dispersion
model is needed to determine the pattern of pollutant distribution and also the maximum concentration
as an effort to estimate or forecast the impacts that can occur. There are two systems that can be used to
model polluters, namely the CALPUFF (California Puff) model and the AERMOD (The American
Meteorology Society Environmental Protection Agency Regulatory Model).
PT. X is an automotive casting factory located in Central Cikarang, Bekasi Regency, West Java.
Production activities at PT.X include pressing, welding, painting, engine assembly, and aftersales. From
the production process, PT. X utilizes combustion or evaporation processes, the by-products of which
are released into the air which have the potential to cause air pollution. Therefore, it is necessary to model
the prediction of pollutant distribution in PT. X to determine the distribution of pollutants and determine
the comparison between the CALPUFF and AERMOD models. To determine the accuracy of the two
models, several types of statistical tests were used, namely correlation coefficient (R), Index of
Agreement (IOA), Fractional Bias (FB), Root Mean Square Error (RMSE), Error, and Mean Bias (MB).
2.
METHODOLOGY
2.1
Secondary Data Collection
Secondary data collection was carried out to assist authors in writing reports on the preparation of
technical approvals for emissions. Secondary data obtained from PT. X in the form of emission
concentration data at the chimney, ambient air data at PT. X. Other data that the author get are
topography, land use data around PT. X, as well as surface and upper air meteorological data in the area
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around PT. X. Topographic data is obtained through the website www.src.com, meteorological data is
obtained through the website www.copernicus.com, and land use data is obtained from global land uses.
2.2
Calculation of Emission Rate
Determination of emission rate is an early stage before conducting modeling. Emission rate is an
important factor that affects the value and pattern of pollutant concentration produced
2.2.1 Calculation of Average Wind Speed
Before calculating the emission rate, it is necessary to calculate the peak speed of the chimney first,
which requires wind speed data from the research location. The average wind speed of the study area is
determined as follows:
π‘Žπ‘£π‘” 𝑀𝑖𝑛𝑑 𝑠𝑝𝑒𝑒𝑑
(π‘šπ‘’π‘‘π‘–π‘Žπ‘› π‘£π‘Žπ‘™π‘’π‘’ 1 π‘₯ % π‘œπ‘“ 𝑀𝑖𝑛𝑑 1) + (π‘šπ‘’π‘‘π‘–π‘Žπ‘› π‘£π‘Žπ‘™π‘’π‘’ 2 π‘₯ % π‘œπ‘“ 𝑀𝑖𝑛𝑑 2) + (π‘šπ‘’π‘‘π‘–π‘Žπ‘› π‘£π‘Žπ‘™π‘’π‘’ 2 π‘₯ % π‘œπ‘“ 𝑀𝑖𝑛𝑑)
=
% π‘‘π‘œπ‘‘π‘Žπ‘™ 𝑀𝑖𝑛𝑑 π‘π‘’π‘Ÿπ‘π‘’π‘›π‘‘π‘Žπ‘”π‘’π‘ 
The average wind speed obtained is 4.52 m/s.
2.2.2 Calculation of Top Chimney Velocity and Emission Rate
Gaussian equations are used to determine stack peak velocity and emission rate. The chimney peak
velocity is obtained through the following equation.
π‘ˆ2
𝑧2 𝑝
=( )
π‘ˆ1
𝑧1
Based on the calculation, the peak velocity of the chimney is 4.77 m/s for scrubber, 4.1 m/s for Dust
Collector 1, and 4.61 um/s for Dust Collector 2. Emission rate of each stacks can be calculated after
getting the top speed at each stack, through the following equation.
πΈπ‘šπ‘–π‘ π‘ π‘–π‘œπ‘› π‘Ÿπ‘Žπ‘‘π‘’ =
𝐢
1
× πœ‹ × π‘‘2 × π‘£
4
Based on the calculation, the velocity at each stack is 2.44 mg/s, 0.38 mg/s, and 0.29 mg/s at the scrubber
stack, 0.73 mg/s, 1.89 mg/s, and 1.54 mg/s at dust collector stack 1, and 0.55 mg/s, 0.67 mg/s, and 0.53
mg/s at dust collector stack 2, for pollutants TSP, SO2, and NO2.
2.3
Determination of Study Area Grid
The study area grid determination is needed to limit the distance over which the pollutant will be
modeled. In this study, a grid of 120 km x 80 km was used with a length of 1 km for each grid.
2.4
Pollutant Dispersion Modeling Using CALPUFF dan AERMOD
The collected data was processed using the CALPUFF AERMOD modeling application. Table 3.6 shows
the differences in input data for CALPUFF and AERMOD.
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Table 2.1 Differences in input data on CALPUFF and AERMOD
The main difference in entering input data in both models is that the user needs to prepare all input data
in CALPUFF before the process continues to the next processor, while empty input data in AERMOD
can be overcome by using the menu to create and generate the data. In AERMOD, the user can choose
which stage to do first. Therefore, using AERMOD is easier and faster than using CALPUFF.
3.
ANALYSIS AND DISCUSSION
3.1 Calculation Results
Table 3.1 shows the results of the emission dispersion of TSP, SO2, and NO2 and the maximum
concentration received by the receptor in the period of 1 and 24 hours.
Table 3.1 The results of the emission dispersion of TSP (left), SO2 (right), and NO2 (bottom) and the
maximum concentrations received by receptors on CALPUFF and AERMOD
Figure 3.1 shows graph mapping of the final and ambient pollutant concentrations.
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Final and Ambien Concentration of SO2
Final and Ambient Concentration of TSP
100
Concentration (µg/m3)
120
Concentration (µg/m3)
100
80
60
40
CALPUFF
20
AERMOD
Data Ambien
0
0
1
2
3
4
5
6
80
CALPUFF
AERMOD
60
Data Ambien
40
20
0
0
1
Sampling Point
2
3
Sampling Point
4
5
6
Final and Ambient Concentration of NO2
Concentration (µg/m3)
70
60
CALPUFF
AERMOD
Data Ambien
50
40
30
20
10
0
0
1
2
3
4
5
6
Sampling Point
Figure 3.1 Graph mapping of the final and ambient pollutant concentrations of TSP (left), SO2 (right),
and NO2 (bottom) on the CALPUFF and AERMOD models
In Figure 3.1, it can be seen that all final concentrations of dispersion have values that are generally
smaller than the ambient data. This can be caused by the use of background concentration data that is not
in accordance with the actual background concentration. Due to the limited background concentration
data sources, the background concentration data used are not entirely correct at the monitoring location
used so that the values may differ from actual conditions. In addition, different actual background
concentration conditions may be caused by location, meteorological conditions, regional development
projections, topography, land use, emission sources, other pollutants in ambient air, and other factors
that have a direct influence on the final dispersion result. In addition, the existence of emission sources
other than PT. X as well as biogenic and natural emissions at the research site which are not considered
in the modeling can also cause dispersion results that are not in accordance with ambient conditions
(Kesarkar et al., 2007).
It is seen that the TSP concentration curve has the same pattern whereas the ambient air concentration
increases, the final dispersion concentration also increases. Likewise, when the ambient concentration
decreases, the final dispersion concentration also decreases. The same pattern also occurs in the SO 2
pollutant mapping curve. However, this pattern was not found in the NO2 pollutant curve. At monitoring
point 3 in Figure 3.1, there is an outlier where the final concentration of the dispersion decreases as the
concentration in the ambient air increases. This condition can be caused by several things such as
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incomplete meteorological data at that point during monitoring time, or differences in background
concentration which causes the final dispersion results to have far differences. But overall, the CALPUFF
model is considered to still be able to predict well according to the pattern in the ambient air even though
the final concentration and dispersion have very large differences in value, CALPUFF and there are also
outliers in NO2 pollutants.
One of the causes of the deviation of the final concentration from the above data with ambient air is due
to the incompleteness of the emission source data (Im U., Yenigun O, 2005). A perfect modeling and
producing precise pollutant predictions according to ambient data depends on the accuracy of the
emission inventory data of the plant concerned and the level of precision of the meteorological and
topographical data at the study site.
Deviations that occur in the validation test of the Gauss model can be caused by the research location
having a complex topography while Gauss's ability is limited to uncomplicated terrain. This happens
because it has a Gaussian Plume base in steady state conditions so it does not consider changes in
meteorological and field conditions in units of space and time. As a result, the AERMOD model is not
suitable for use in research sites with complex terrain, changing meteorological conditions because the
results will have values that are far from the ambient data. This is in accordance with the terrain
conditions in Bekasi Regency which have different land heights with a range of 3-40 meters above sea
level so that the Bekasi Regency terrain becomes complex. (BPS Bekasi Regency, 2022). In particular,
Cikarang Sub-district in Bekasi Regency has a topography of 15-46 mdpl, so that the meteorological data
available under these conditions is highly variable. This condition explains the deviation of the final
concentration values in AERMOD and CALPUFF.
Meteorological conditions can also cause data deviation on AERMOD, where AERMOD cannot model
pollutants with wind speeds <1 m/s (Masuraha, 2006). Based on surface meteorological data, there are
winds with a speed of <1 ms which are called calm winds as much as 2% during the research period.
This condition can explain the deviations made by the AERMOD model in modeling the three types of
pollutants at PT. X.
3.2
Statistics Test
Data for statistical test is the final concentration of dispersion data by CALPUFF and AERMOD and
ambient air concentration. Statistical tests were carried out by comparing the final concentration of the
dispersion with the concentration in ambient air at the same coordinate point.
The statistical test shows that CALPUFF has a higher accuracy than AERMOD in predicting the
concentration for each pollutant, as evidenced by the statistical test value of CALPUFF which tends to
be higher than AERMOD.
4.
CONCLUSION
Based on the research conducted, it can be concluded as follows:
1. CALPUFF has a Lagrangian non-steady state basis while AERMOD has a Gasussian Plume steady
state basis so that the difference in the prediction results of concentrations in the air.
2. CALPUFF is able to model concentration predictions more accurately than AERMOD because
CALPUFF pays attention to the reaction of each particle after it is dispersed, takes into account variations
in meteorological and topographical conditions in the study area at the time of observation, is able to
make predictions at each point and at certain hours, and takes into account the presence of calm winds
at the time of observation.
3. The statistical test proves that CALPUFF has more capabilities than AERMOD because the test results
are higher than the AERMOD test results.
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5.
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