Impact of anthropogenic emissions on biogenic secondary organic aerosol: observation in the Pearl River Delta, southern China
<p>Secondary organic aerosol (SOA) formation from biogenic precursors is affected by anthropogenic emissions, which are not well understood in polluted areas. In this study, we accomplished a year-round campaign at nine sites in polluted areas located in the Pearl River Delta (PRD) region duri...
Main Authors: | , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2019-11-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/19/14403/2019/acp-19-14403-2019.pdf |
Summary: | <p>Secondary organic aerosol (SOA) formation from biogenic precursors
is affected by anthropogenic emissions, which are not well understood in
polluted areas. In this study, we accomplished a year-round campaign at nine
sites in polluted areas located in the Pearl River Delta (PRD) region during
2015. We measured typical biogenic SOA (BSOA) tracers from isoprene,
monoterpenes, and <span class="inline-formula"><i>β</i></span>-caryophyllene, as well as major gaseous and
particulate pollutants and investigated the impact of anthropogenic
pollutants on BSOA formation. The concentrations of BSOA tracers were in the
range of 45.4 to 109 ng m<span class="inline-formula"><sup>−3</sup></span> with the majority composed of products from
monoterpenes (SOA<span class="inline-formula"><sub>M</sub></span>, <span class="inline-formula">47.2±9.29</span> ng m<span class="inline-formula"><sup>−3</sup>)</span>,
isoprene (SOA<span class="inline-formula"><sub>I</sub></span>, <span class="inline-formula">23.1±10.8</span> ng m<span class="inline-formula"><sup>−3</sup>)</span>, and <span class="inline-formula"><i>β</i></span>-caryophyllene (SOA<span class="inline-formula"><sub>C</sub></span>, <span class="inline-formula">3.85±1.75</span> ng m<span class="inline-formula"><sup>−3</sup>)</span>. We found that
atmospheric oxidants, <span class="inline-formula">O<sub><i>x</i></sub></span> (<span class="inline-formula">O<sub>3</sub></span> plus <span class="inline-formula">NO<sub>2</sub></span>), and sulfate
correlated well with later-generation SOA<span class="inline-formula"><sub>M</sub></span> tracers, but this was not the case for
first-generation SOA<span class="inline-formula"><sub>M</sub></span> products. This suggested that high <span class="inline-formula">O<sub><i>x</i></sub></span> and
sulfate levels could promote the formation of later-generation SOA<span class="inline-formula"><sub>M</sub></span> products,
which probably led to the relatively aged SOA<span class="inline-formula"><sub>M</sub></span> that we observed in the PRD. For
the SOA<span class="inline-formula"><sub>I</sub></span> tracers, both 2-methylglyceric acid (NO/<span class="inline-formula">NO<sub>2</sub></span>-channel
product) and the ratio of 2-methylglyceric acid to 2-methyltetrols
(<span class="inline-formula">HO<sub>2</sub></span>-channel products) exhibit <span class="inline-formula">NO<sub><i>x</i></sub></span> dependence, indicating the
significant impact of <span class="inline-formula">NO<sub><i>x</i></sub></span> on SOA<span class="inline-formula"><sub>I</sub></span> formation pathways. The
SOA<span class="inline-formula"><sub>C</sub></span> tracer was elevated in winter at all sites and was positively correlated
with levoglucosan, <span class="inline-formula">O<sub><i>x</i></sub></span>, and sulfate. Thus, the unexpected increase in
SOA<span class="inline-formula"><sub>C</sub></span> in wintertime might be highly associated with the enhancement of
biomass burning, <span class="inline-formula">O<sub>3</sub></span> chemistry, and the sulfate component in the PRD. The
BSOAs that were estimated using the SOA tracer approach showed the highest
concentration in fall and the lowest concentration in spring with an annual
average concentration of <span class="inline-formula">1.68±0.40</span> <span class="inline-formula">µ</span>g m<span class="inline-formula"><sup>−3</sup></span>. SOA<span class="inline-formula"><sub>M</sub></span>
dominated the BSOA mass all year round. We also found that BSOA correlated
well with sulfate and <span class="inline-formula">O<sub><i>x</i></sub></span>. This implied a significant effect from
anthropogenic pollutants on BSOA formation and highlighted that we could
reduce BSOA by controlling the anthropogenic emissions of
sulfate and <span class="inline-formula">O<sub><i>x</i></sub></span> precursors in polluted regions.</p> |
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ISSN: | 1680-7316 1680-7324 |