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Characterization of inorganic species and carboxylic acids in
ambient aerosol during dry season in the Chiang Mai Basin,
ThailandA. Chotruksa1, Hsin-ChingWu, Y.I. Tsai2, K. Sopajaree1
1. Department of Environmental Engineering, Chiang Mai University, Chiang Mai 50200, Thailand2. Department of Environmental Engineering and Science, Chia Nan University of Pharmacy and
Science, 60, Sec. 1, Erh-Jen Rd., Jen-Te, Tainan 717, Taiwan
Abstract
Aerosol samples for PM10 were collected during dry season of February and
April at two sites different sampling locations in Chiang Mai basin, Thailand.
Concentrations of water-soluble inorganic species and carboxylic acids in PM10 were
quantified. Oxalic acid was the dominant dicarboxylic acid species, follow by maleic
acid. Mass ratio of acetic to formic acids (A/F) > 1 was often used to demonstrate theprimary source by wood burning or vehicular emission, and it indicated that the
contribution of primary sources was higher at suburban site than urban site.
Carboxylic acid concentration during the PM10 episode is higher than that during
non-episodic period. The most significant contribution to PM10 in Chiang Mai basin
was from the photochemical formation of secondary aerosols and biomass burning.
Keywords: Carboxylic acids; Maleic acid; A/F ratio
Table 1. Title
Figure 1. title
0
2
4
6
8
10
12
0 2 4 6
X ( unit)
Y
(unit)
s rac
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1. Introduction
Particulate matter is the major air pollutant of atmospheric aerosols and can be
the predominant constituent of find atmospheric particles, are important organics
resulting from the marine pathway, biomass burning, agriculture burning, automotiveexhaust emission and anthropogenic emission (Khwaja, 1995; Chebbi and Carlier,
1996; Souza et al., 1999; Hsieh et al., 2008; Lee et al., 2008; Zhang et al., 2008;).
These emissions are impacts on regional air quality and visibility, ecosystems and
human health, and climate change (Khwaja, 1995; Souza et al., 1999; Tsai, 2005).
Low molecular weight carboxylic acids are ubiquitous and important
components in the tropospheric aqueous and gaseous phases, and in aerosol particles
(Chebbi and Carlier, 1996). Carboxylic acids in the particle phase accounted for a
small fraction of the organic carbon. Results indicated that photochemical processes
and anthropogenic emissions such as automobile exhaust are major sources of
atmospheric carboxylic acids (Khwaja, 1995). Monocarboxylic acids were observedwith a daytime maximum and a nighttime minimum (Khawaja, 1995; Chebbi and
Carlier, 1996). Formic and acetic acids constitute the most abundant carboxylic acids
in the global troposphere (Khwaja, 1995; Souza et al., 1999). During daytime,
vehicular emission appeared to be the primary source of acetic acid, whereas formic
and pyruvic acids should be formed photochemically (Souza et al., 1999). In addition,
formic acid is one of the photochemical oxidation products from volatile organic
compounds (VOC), the results show that 80-100% of formic acid stems from biogenic
VOC emitted from terrestrial sources (Glasius et al., 2000). Besides that, dicarboxylic
acids are among the most abundant organic constituents of ambient particulate matter
(Ray and McDow, 2005). Dicarboxylic acids are widely present in the urban, rural
and marine atmosphere. Oxalic acid was found as the most abundant species,
followed by succinic and malonic (Khawaja, 1995; Chebbi and Carlier, 1996; Ho et
al., 2006; Hsieh et al., 2008; Tsai et al., 2008; Hsieh et al., 2009).
The biomarker levoglucosan (1,6-anhydro--D-glucopyranose) is formed as a
result of the thermal breakdown alteration of the cellulose, accompanied by generally
lesser amounts of straight-chain, aliphatic and oxygenated compounds and terpenoids
present in the vegetation subjected to biomass burning. The biopolymer (cellulose)
decomposes during combustion, yielding a tarry material containing anhydrosugars
(Simoneit et al.,1999; Santos et al., 2002; Lee et al., 2008). This compound, together
with other thermal decomposition products from cellulose and hemicelluloses (e.g.manosan, galactosan and levoglucosan) were utilized as tracers for biomass burning
(Santos et al., 2002; Schmidl et al., 2008; Bari et al., 2009; Caseiro et al., 2009; Fabbri
et al., 2009). It has a large impact on the biomass burning attribution as it is emitted
at high concentrations. (Simoneit et al., 1999; Jordan et al., 2006; Zhang et al., 2008).
Moreover, Jordan et al., (2006) reported that woodsmoke was estimated to comprise
about 95% of wintertime air pollution in Launceston, and the resulting average
levoglucosan woodburning emission factor of around 140 mg g-1 particulate matter
was found to be consistent with previously determined woodheater emissions.
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2. Methodology
2.1 Sampling
Aerosol samples were collected on a 47-mm Teflon filters(Zefluor, Pall) using a
Ecotech MicroVol 1100 Particulate Sampler with a total flow rate of 3 L min-1,
between 2 February-2 April 2010, at two sites: Facultyof Architecture Chiang MaiUniversity (CMU; Located at latitude 18o4754.90 N and longitude 98o5655.75 E),
set at a height of 12 m above ground, located in the urban area, has little traffic, near
Suthep mountain and excellent ventilation; TOT Public Company Limited (TOT;Located at latitude 18o 41 40.04 N and longitude 99o2' 59.45 E), set at ground
level, with heavy traffic highways and close to the industrial zone. Each sampling
collected two sets of aerosol samples were collected daily, one from 7 am to 7 pm
(12 h: daytime) every 3 days and another from 7 pm to 7 am (12 h: nighttime)
every 3 days.
The geographic locations of air samplings are shown in Figure 2.1.
Figure 2.1 Map of Chiang Mai province area identifying the location of air sampling
sites.
2.2 Sampling handing
Before and after sample collection, filters were conditioned at 405% RH for
24 hours and subsequently weighed at 503% RH using a Mettler Toledo AT261
analytical balance with a sensitivity of 10 g and a Sartorius CP2P analytical balance
with a sensitivity of 1 g. All weight measurements were repeated three or more times
and the Shewart control procedures were followed to ensure reliability. Additionally,
blank filters were prepared by purging in 99.995% pure nitrogen for 30 seconds and
then processed as for sample-containing filters.
2.3 Chemical analysis and quality assurance
CMU site
TOT site
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The sample-containing filters, unexposed blanks will be stored in petri dishes
placed inside an unlit refrigerator below -18C to prevent loss of semi-volatile species,
especially carboxylic acids and ammonium nitrate. For analyzing carboxylic acid,
cations and anions, the filter paper will be placed in a PE bottle, 10.0 mL of deionized
water (resistivity >18.0 M cm-1 at 25C, Barnstead) will be added and the contents
will be shaken (Yihder TS-500 Shaker) in an unlit refrigerator at 4 C for 90 min toprevent the decomposition of the extracted carboxylic acid species. The liquid is then
filtered through a 0.2 m ester acetate filter and the aqueous filtrate will be is
characterized using IC, following a slightly modified version of the method of Hsieh
et al. (2008).
The ion chromatography system (IC) model DX-600, Dionex is equipped with a
gradient pump (Model GP50), an ASRS-Ultra anion self-regenerating suppressor, a
conductivity detector (CD25), a Spectrasystem automated sampler (AS3500) with 2
mL vials, and a Teflon injection valve using a 1000 L sample loop, in combination
with analytical column and Ion Pac AG11-HC, AS-11-HC (4 mm), eluent for the DI
water (deionized), 5 mM NaOH, 100 mM NaOH and 100% MeOH gradient elution
method to conduct analysis. The flow rate is maintained at 2.0 mL min-1 during the
carboxylic acid analyses, which Ion Chromatography Dionex DX-600 gradient elution.
This method allows for the analysis of acetic acid, formic acid, glutaric acid, succinic
acid, malic acid, malonic acid, tartaric acid, maleic acid, fumaric acid, oxalic acid,
phthalic acid and citric acid in the aerosol samples.
Additionally, 1000 L of the aqueous extract will be injected into IC Model
Dionex ICS-2500 using 9 mM Na2CO3 eluent at a flow rate of 1.4 mL min-1.
Concentrations of the separated inorganic species including Cl-, NO3- and SO4
2-, are
determined in analytical column RFIC
TM
Ion Pac AS14A, AG14A (4 mm). Cationsystem to IC Model Dionex ICS-1000, AS1000, analytical column and Ion Pac
CG12A, CS12A (4 mm), injection volume 25 L and an isocratic 20 mM MSA
(CH4O3S) eluent at a flow rate of 1.0 mL min-1 will be used for determination of
cations, including Na+, NH4+, K+, Mg2+ and Ca2+. Department of anhydrosugars
(levoglucosan, mannosan and galactosan) are to IC Model Dionex ICS-2500 (ED50,
GP50, AS50), analytical column and Carbo PacTM MA1 (4 mm), flow rate 0.4
mL/min, injection volume 0.2 mL, eluent conducted for the 400 mM NaOH
component analysis.
All reagents are of analytical grade, obtained from Merck (Darmstadt, Germany),
and are used without further purification. The solutions will be prepared usingdeionized water from which organic carbon had been removed and the detection
limits corresponded to 10-50 ng for the carboxylic acids investigated.
2.4 Other data
Ambient air quality data were obtained from the Thailand Pollution Control
Department (PCD), information was obtained on Air Quality data from 2 February to
2 April 2010 over Chiang Mai province, Thailand. The Air Quality was particularly
useful for observing pollutant concentrations. Moreover visibility was obtained from
Thai Meteorological Department during sampling.
Site meteorological data (Table 1) confirm designations of each period of
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study. In this study to explain two period was the non-episodic pollution period
(PM10120 g m
-3). During the PM10
episode and non-episodic pollution period, average PM10 concentrations were 156.88
38.10 and 78.71 20.42 g m-3, respectively. The data shows concentrations of
pollutant, especially O3, SO2, NO2, NOx, NO and CO, which represent traffic
emission, were higher during the PM10 episode. Moreover, higher temperature, lowerrelative humidity and lower wind speed during the PM10 episode to be high O3 is due
to lower visibility, higher PM10 and increase pollutant of these periods.
3. Results and discussion
3.1 Carboxylic acids
The water soluble organic acids, accessible by ion chromatography, were
monocarboxylic acids (acetic acid and formic acid), dicarboxylic acids and
tricarboxylic acids. The most abundant carboxylic acids at the CMU site (urban) and
TOT site (suburban) was oxalic acid, follow by acetic acid and maleic acid during the
PM10 episode, while during non-episodic pollution period acetic acid was the most
abundant species, follow by oxalic acid and maleic acid (see Figure 1). Sources of
maleic acid from wood and coal burning was the dominant source in the Christchurch
wintertime (Wang et al.,2004) indicated that source in Chiang Mai may be from wood
burning.
During the PM10 episode, carboxylic acids higher during daytime indicating
that carboxylic formed by photochemical reaction and/or emitted directly by fossil
fuels and biomass burning processes more frequency at daytime. At the CMU site the
concentrations of carboxylic acids higher than TOT site. Moreover, Formic-to-acetic
acid ratio (A/F) (see Tables 2 and 3) was used to distinguish the primary (A/F>1) andthe secondary (A/F
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3.3 Relationships among chemical species during non-episodic pollution period
and PM10 episode at TOT site
Varimax-rotated principal component analysis was used in this study to
investigate the various sources of air pollution. Table 4 lists the Factors results fordaily PM10 chemical composition, air pollutants and relative humility temperature and
wind speed during non-episodic pollution and PM10 episode at TOT site. During
non-episodic pollution, there were six factors with eigenvalues exceeding 1.0
indicating that these factors had a significant influence on the air quality of this
period. They account for 88.9% of explained variance of air quality. The variance that
can be explained by the first Factor (Factor 1) is 30.1% and the significant component
loading (component loading 0.7) is mainly related primary source species including
acetic and fumaric acid. Additionally during non-episodic pollution sea salts, i.e.
sodium and calcium but at Chiang Mai is more than 600 km inland of the shore may
be source from some industrial. And, ammonium from traffic emission has strong
correlation. Hence, as mentioned in the literature (Hsieh et al., 2008; Tsai and Cheng,2004; Tsai and Chen, 2006). Factor 2, which explain source from photochemical
oxidation of oxalic and succinic acid. Good correlation with potassium and sulfate
indicated that source from biomass or traffic emission. Glutaric, maleic and citric acid
and nitrate are strongly positively correlated in Factor 3, indicated that source from
traffic emission. In Factor 4, good correlation with calcium and tartaric acid, showing
that the contributed from traffic and coal combustion. During PM10episode, calcium,
nitrate and acetic acid in Factor 1 display significant component loading confirming
that primary source from traffic emission. Factor 2, tartaric, maleic and fumaric acid
contributed from traffic emission or coal burning. In Factor 3, glutaric, succinic and
malonic show component loading indicating the influence of photochemical or
secondary source from traffic. Factor 7, malic acid high correlation with phthalic acid
implies that the atmospheric environment is affected by emission from biomass
burning activities. Sodium and chloride in Factor 8 showing that the sea breeze to
contribute to the atmosphere or may be from industrial area.
4 Conclusion
This study has investigated the water-soluble carboxylic acid species in PM10
aerosols in Chiang Mai basin. Some principal conclusions were presented as follows:
(1)The most abundant carboxylic acids at the CMU site (urban) and TOT site
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(suburban) was oxalic acid, follow by acetic acid and maleic acid during the
PM10 episode, while during non-episodic pollution period acetic acid was the
most abundant species, follow by oxalic acid and maleic acid
(2)Acetic-to-formic acid ratio (A/F) > 1 was often used to distribute fromprimary source by wood burning or vehicular emission, and it indicated that
the contribution of primary sources from biomass burning, was higher at TOTsite than CMU site.
(3)During the PM10 episode, carboxylic acids higher during daytime indicatingthat carboxylic formed by photochemical reaction and/or emitted directly by
fossil fuels and biomass burning processes more frequency at daytime.
(4)At TOT site, most abundant source emission from traffic and coal burning.
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Table 1 Meteorological and related air pollution information during the period of
study at the suburban site
ParameterDuring non-episodic
pollution
During the PM10episode
Mean SD Mean SD
Temperature ( C) 25.61 3.38 28.49 2.65
Relative humidity (%) 54.07 7.88 52.11 7.09
Pressure (mmHg) 731.17 1.56 731.92 1.38
Visibility (km) 8.21 1.24 5.80 1.38
Prevailing wind
directionNW-N NW-N
Wind speed 1.68 0.54 1.60 0.43
PM10 (g m-3) 78.71 20.42 156.88 38.10
O3 (ppb)a
49.06 29.42 90.86 31.21SO2 (ppb) 0.70 0.41 1.53 0.46
NO2 (ppb) 14.64 5.34 14.69 3.12
NOx (ppb) 19.78 7.44 17.94 2.56
NO (ppb) 5.16 2.61 3.30 1.11
CO (ppm) 0.78 0.19 1.11 0.26a Average maximum hourly ozone in each sampling sets.
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Table 2 Mean (SD) chemical composition of PM10 aerosol and ratios of species nighttime/daytime concentrations during non-episodic pollution
period and PM10 episode at CMU site.
Species
CMU site
During non-episodic pollution period During PM10 episode
Mean SD Mean SD
PM10 (g m-3) 58.08 30.85 1.04 1.10 139.56 13.97 0.921 0.458
Inorganic species (g m-3) 7.15 4.09 1.54 0.94 15.12 4.41 0.83 0.93
Sodium 0.48 0.49 1.49 1.35 1.19 1.04 0.881 0.886
Ammonium 1.23 0.89 1.57 1.85 2.71 0.79 1.109 2.032Potassium 0.89 0.57 1.40 1.10 2.31 0.56 1.043 2.075
Magnesium 0.31 0.30 2.27 3.78 0.73 0.28 1.111 1.172
Calcium 0.92 0.61 1.11 2.03 1.88 0.67 0.633 0.418
Chloride 0.25 0.15 1.22 0.80 0.55 0.74 0.296 0.050
Nitrate 1.22 1.01 1.81 2.33 2.10 1.94 0.533 0.222
Sulfate 1.84 1.36 1.45 1.24 3.65 1.03 1.062 2.455
Carboxylic acids (ng m-3) 1109.30 480.28 1.05 0.60 2148.35 1010.58 0.69 0.53
Acetic acid 325.14 274.39 1.71 1.47 443.16 489.92 0.257 0.373
Formic acid 55.28 39.60 1.84 2.29 148.07 156.73 0.555 0.403
Glutaric acid 18.59 27.93 0.40 0.30 57.87 32.53 0.843 0.938
Succinic acid 36.40 37.55 0.68 0.72 105.73 51.68 0.747 0.836
Malic acid 61.51 55.87 1.23 1.46 144.66 70.10 0.685 0.593
Malonic acid 48.76 27.43 0.88 0.86 99.54 32.50 0.731 0.988Tartaric acid 39.12 60.19 0.55 0.26 54.33 23.80 1.044 1.953
Maleic acid 141.13 153.71 0.96 0.95 151.91 194.25 0.828 0.339
Fumaric acid 9.38 7.52 0.77 0.64 27.38 13.92 0.706 1.235
Oxalic acid 284.32 207.48 1.17 1.13 758.87 198.82 0.865 1.264
Phthalic acid 29.06 24.01 1.83 1.34 51.39 35.44 0.843 1.281
Citric acid 60.59 76.16 0.61 0.28 105.43 179.31 0.131 0.072
Acetic/Formic 5.88 6.93 2.99 3.13
Malonic/Succinic 1.34 0.73 0.9 0.6
daytime
nighttime
daytime
nighttime
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Table 3 Mean (SD) chemical composition of PM10 aerosol and ratios of species nighttime/daytime concentrations during non-episodic pollution
period and PM10 episode at TOT site.
Species
TOT site
During non-episodic pollution period During PM10 episode
Mean SD Mean SD
PM10 (g m-3) 76.54 25.86 0.82 0.57 141.21 17.85 0.97 1.20
Inorganic species (g m-3) 7.14 3.76 1.66 5.05 13.18 4.41 0.96 1.02
Sodium 0.50 0.74 2.67 12.22 0.64 0.75 0.83 2.05
Ammonium 0.84 0.58 1.41 2.12 2.01 0.70 0.99 0.94Potassium 0.75 0.36 1.33 1.23 1.87 0.54 0.99 0.76
Magnesium 0.25 0.10 1.01 0.72 0.55 0.26 0.69 0.65
Calcium 1.24 0.47 0.89 0.55 2.05 0.83 0.84 0.30
Chloride 0.39 0.52 2.78 12.10 0.46 0.49 1.48 3.20
Nitrate 1.94 1.53 1.71 1.81 2.39 2.08 0.84 0.27
Sulfate 1.22 0.79 1.48 1.47 3.20 1.05 1.05 1.73
Carboxylic acids (ng m-3) 1068.12 431.43 1.37 1.24 1783.01 782.56 0.81 0.41
Acetic acid 408.24 265.03 1.49 3.73 467.98 341.65 0.54 0.46
Formic acid 43.64 31.69 1.29 2.71 54.13 35.99 1.17 1.31
Glutaric acid 8.45 7.35 1.73 2.50 37.75 24.60 0.99 0.87
Succinic acid 22.86 16.44 0.76 0.70 70.07 32.37 0.88 1.38
Malic acid 52.23 41.67 1.48 2.83 107.25 70.79 0.70 0.51
Malonic acid 39.58 14.19 0.78 1.30 78.09 23.78 0.97 0.93Tartaric acid 28.51 37.66 0.56 0.47 46.87 28.42 0.98 0.96
Maleic acid 176.28 161.99 3.49 3.94 210.41 475.75 0.38 0.15
Fumaric acid 5.53 3.60 1.18 0.92 18.99 15.97 0.87 0.71
Oxalic acid 215.62 76.31 1.10 0.82 591.81 174.10 0.99 0.73
Phthalic acid 21.75 20.64 0.97 0.75 35.93 26.03 0.72 1.26
Citric acid 45.43 47.78 1.66 1.42 63.72 144.17 0.45 0.23
Acetic/Formic 9.35 8.36 8.65 9.49
Malonic/Succinic 1.73 0.86 1.11 0.73
daytime
nighttime
daytime
nighttime
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Table 4 Varimax-rolated principal component loading of daily PM10 chemical species pollutants and relative humidity, temperature and wind speed
during non- episodic pollution period and PM10 episode
TOT during non-episodic pollution period TOT during the PM10 episode
Factor1 Factor2 Factor3 Factor4 Factor5 Factor6 Factor1 Factor2 Factor3 Factor4 Factor5 Factor6 Factor7 Factor8
Variance
PM10 0.03 0.76 -0.14 0.41 0.34 0.00 -0.08 -0.30 0.07 -0.18 0.20 -0.85 0.07 0.08
Sodium 0.94 0.03 -0.01 -0.14 0.12 0.11 -0.04 0.10 0.14 0.07 0.12 0.00 0.10 0.92
Ammonium 0.72 0.17 0.52 0.26 -0.18 0.27 0.49 -0.20 0.21 -0.48 0.40 0.47 0.06 0.17
Potassium 0.37 0.90 0.02 -0.08 -0.01 -0.08 0.15 -0.45 0.55 -0.16 0.26 0.02 0.06 0.45
Magnesium 0.39 0.33 0.33 0.65 -0.14 0.08 0.64 -0.23 0.45 0.14 0.39 0.16 0.26 -0.13
Calcium 0.14 0.43 0.31 0.74 -0.03 0.15 0.90 -0.11 0.22 -0.10 0.15 0.03 -0.08 -0.17
Chloride 0.95 0.21 0.14 -0.05 0.00 0.10 -0.12 0.10 0.26 -0.27 -0.02 -0.06 0.08 0.88Nitrate 0.26 0.11 0.88 0.27 -0.22 -0.03 0.85 0.10 0.32 -0.28 -0.04 -0.05 -0.12 -0.15
Sulfate 0.14 0.84 0.30 0.02 -0.32 0.09 0.25 -0.20 -0.16 -0.63 0.35 0.01 -0.31 0.31
Acetic acid 0.76 0.33 0.06 0.04 0.05 -0.40 0.84 0.00 -0.08 0.20 0.24 0.11 -0.18 0.23
Formic acid 0.41 0.32 0.61 0.11 0.24 0.05 -0.38 0.38 0.60 -0.03 0.08 0.22 -0.10 0.24
Glutaric acid -0.27 0.25 0.82 0.08 0.13 -0.15 0.05 0.54 0.71 0.07 -0.12 0.03 0.26 0.25
Succinic acid -0.40 0.76 -0.28 0.16 0.32 -0.15 0.21 0.11 0.90 0.01 0.02 -0.19 0.10 0.14
Malic acid 0.22 0.05 0.04 -0.18 0.88 -0.01 -0.04 0.26 0.03 0.13 -0.13 -0.18 0.82 0.20
Malonic acid -0.45 0.28 0.11 0.62 0.22 -0.43 0.31 0.04 0.90 0.04 0.09 0.05 0.06 0.13
Tartaric acid -0.11 -0.25 0.48 0.78 -0.08 0.05 -0.09 0.71 0.43 0.15 -0.29 -0.14 -0.22 0.05
Maleic acid 0.02 0.00 0.91 -0.15 -0.13 0.12 -0.07 0.95 0.06 0.06 0.10 0.11 0.08 0.05
Fumaric acid 0.76 0.29 -0.06 0.12 0.26 -0.04 0.22 0.78 -0.02 -0.25 0.18 0.13 0.10 0.17
Oxalic acid 0.34 0.90 0.11 0.14 0.04 -0.04 0.25 -0.58 0.61 0.02 0.25 0.18 0.07 0.05
Phthalic acid -0.13 0.04 -0.10 -0.17 -0.01 -0.89 -0.34 -0.08 0.40 0.11 0.23 0.15 0.73 0.07
Citric acid 0.16 -0.26 0.83 0.27 0.26 0.12 -0.07 0.96 0.07 0.10 0.00 0.10 0.07 0.01
RH 0.30 -0.35 0.51 -0.55 0.18 -0.10 -0.20 -0.22 -0.02 0.11 -0.85 0.19 0.28 -0.08
Temp. 0.12 -0.02 -0.43 0.68 -0.19 0.36 0.15 -0.08 0.10 0.19 0.89 0.00 0.23 0.06
Wind speed 0.67 -0.55 0.00 0.21 0.18 0.32 0.01 0.01 0.05 0.94 0.18 0.14 0.08 -0.05
Eigenval 7.23 4.72 3.94 2.85 1.56 1.04 5.84 5.07 3.08 2.48 1.94 1.21 1.10 1.02
% total Variance 30.11 19.65 16.41 11.86 6.52 4.33 24.34 21.13 12.83 10.33 8.10 5.03 4.58 4.27
Cumul. Eigenval 7.23 11.94 15.88 18.73 20.29 21.33 5.84 10.91 13.99 16.47 18.41 19.62 20.72 21.75
Cumul. % 30.11 49.76 66.17 78.03 84.55 88.89 24.34 45.46 58.29 68.62 76.72 81.76 86.34 90.61
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a
b
Figure 1 Concentration mean carboxylic acids at two sites during daytime and
nighttime (a) Non-episodic pollution period (b) PM10 episode.
TOT site during Non - episodic pollution period
Carboxylic acids
Acetica
cid
Formic
acid
Glutari
cacid
Succini
cacid
Malica
cid
Maloni
cacid
Tartari
cacid
Maleic
acid
Fumaric
acid
Oxalica
cid
Phthali
cacid
Citrica
cid
Concentration(ngm-3)
0102030405060708090
100110120200
300
400
500
600
700
800
900
1000
Daytime (PM10 mass conc.= 86.03 +/- 34.11 g m-3)Nighttime (PM10 mass conc.= 70.60 +/- 19.41 g m-3)
TOT site during PM10
episode
Carboxylic acids
Acetica
cid
Formic
acid
Glutari
cacid
Succini
cacid
Malica
cid
Maloni
cacid
Tartari
cacid
Maleic
acid
Fumaric
acid
Oxalica
cid
Phthali
cacid
Citrica
cid
Concentration(ngm-3)
0
50
100
150
200
250
300
500
600
700
800
900
1000
1100
1200
1300
Daytime (PM10
mass conc.= 143.39 +/- 16.62g m-3)Nighttime (PM
10mass conc.= 139.02 +/- 19.89g m-3)
CMU site during PM10
episode
Carboxylic acids
Acetica
cid
Formic
acid
Glutari
cacid
Succini
cacid
Malica
cid
Maloni
cacid
Tartari
cacid
Maleic
acid
Fumaric
acid
Oxalica
cid
Phthali
cacid
Citrica
cid
Concentration(ngm-3)
0
100
200
300
400
800
1000
1200
1400Daytime (PM
10mass conc.= 145.27 +/- 17.19g m-3)
Nighttime (PM10
mass conc.= 133.86 +/- 7.88g m-3)
CMU site during Non - episodic pollution period
Carboxylic acids
Acetica
cid
Formic
acid
Glutari
cacid
Succini
cacid
Malica
cid
Malonic
acid
Tartari
cacid
Maleic
acid
Fumaric
acid
Oxalica
cid
Phthali
cacid
Citrica
cid
Concentration(ngm-3)
0
20
40
60
80
100
120
140
160
180
300
400500
600
700
800
900
1000
Daytime (PM10 mass conc.= 56.94 +/- 30.26 g m-3)Nighttime (PM10 mass conc.= 59.35 +/- 33.29 g m-3)