Characterization of carbonaceous aerosols in Singapore: insight from black carbon fragments and trace metal ions detected by a soot particle aerosol mass spectrometer
<p>Understanding sources and atmospheric processes that can influence the physiochemical properties of carbonaceous aerosols is essential to evaluate their impacts on air quality and climate. However, resolving the sources, emission characteristics, and aging processes of carbonaceous aerosols...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-05-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/20/5977/2020/acp-20-5977-2020.pdf |
Summary: | <p>Understanding sources and atmospheric processes that can influence
the physiochemical properties of carbonaceous aerosols is essential to
evaluate their impacts on air quality and climate. However, resolving the
sources, emission characteristics, and aging processes of carbonaceous
aerosols in complex urban environments remains challenging. In this work, a
soot particle aerosol mass spectrometer (SP-AMS) was deployed to
characterize organic aerosols (OAs), refractory black carbon (rBC), and trace metals in
Singapore, a highly urbanized city with multiple local and regional air
pollution sources in the tropical region. rBC (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">C</mi><mn mathvariant="normal">1</mn><mo>+</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="16pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="472eb161d64b68a231d325ff11f4c3a5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-5977-2020-ie00001.svg" width="16pt" height="15pt" src="acp-20-5977-2020-ie00001.png"/></svg:svg></span></span>–<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">C</mi><mn mathvariant="normal">9</mn><mo>+</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="16pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="8af7b9817e69df4fd53090a915849774"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-5977-2020-ie00002.svg" width="16pt" height="15pt" src="acp-20-5977-2020-ie00002.png"/></svg:svg></span></span>)
fragments and trace metal ions (<span class="inline-formula">K<sup>+</sup></span>, <span class="inline-formula">Na<sup>+</sup></span>, <span class="inline-formula">Ni<sup>+</sup></span>, <span class="inline-formula">V<sup>+</sup></span>, and
<span class="inline-formula">Rb<sup>+</sup></span>) were integrated into our positive matrix factorization of OA. Two
types of fossil fuel combustion-related OAs with different degrees of
oxygenation were identified. This work provides evidence that over 90 % of
rBC originated from local combustion sources with a major part related
to traffic and <span class="inline-formula">∼30</span> % associated with fresh
secondary organic aerosol (SOA) produced under the influence of shipping
and industrial emission activities (e.g., refineries and petrochemical
plants) during daytime. The results also show that <span class="inline-formula">∼43</span> % of
the total rBC was emitted from local traffic, while the rest of the rBC fraction
stemmed from multiple sources including vehicular sources, shipping, and industrial
emissions, but was not fully resolved. There was only a weak association
of the cooking-related OA component with rBC. Although there was no
observable biomass burning episode during the sampling period, <span class="inline-formula">K<sup>+</sup></span> and
<span class="inline-formula">Rb<sup>+</sup></span> were mainly associated with the more oxidized oxygenated OA
component, indicating the potential contribution of regional biomass burning
and/or coal combustion emissions to this aged OA component. Furthermore, the
aerosol pollutants transported from the industrial area and shipping ports
presented higher <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M12" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msubsup><mi mathvariant="normal">C</mi><mn mathvariant="normal">1</mn><mo>+</mo></msubsup><mo>/</mo><msubsup><mi mathvariant="normal">C</mi><mn mathvariant="normal">3</mn><mo>+</mo></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="36pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="aeff7c7aa7fbabf3ed61ae9da0262ad8"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-5977-2020-ie00003.svg" width="36pt" height="15pt" src="acp-20-5977-2020-ie00003.png"/></svg:svg></span></span> and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M13" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi mathvariant="normal">V</mi><mo>+</mo></msup><mo>/</mo><msup><mi mathvariant="normal">Ni</mi><mo>+</mo></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="38pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="03c39fb5ab0d7aa899626939f16010da"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-5977-2020-ie00004.svg" width="38pt" height="14pt" src="acp-20-5977-2020-ie00004.png"/></svg:svg></span></span> ratios than
those associated with traffic. The observed association between <span class="inline-formula">Na<sup>+</sup></span> and
rBC suggests that the contribution of anthropogenic emissions to total
particulate sodium should not be ignored in coastal urban environments.
Overall, this work demonstrates that rBC fragments and trace metal ions can
improve our understanding of the sources, emission characteristics, and
aging history of carbonaceous aerosol (OA and rBC) in this type of complex
urban environment.</p> |
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ISSN: | 1680-7316 1680-7324 |