Measurement report: Intensive biomass burning emissions and rapid nitrate formation drive severe haze formation in the Sichuan Basin, China – insights from aerosol mass spectrometry
Haze pollution is a severe environmental problem, caused by elevation of fine particles (aerodynamic diameter <2.5 µm, PM2.5), which is related to secondary aerosol formation, unfavourable synoptic conditions and regional transport, etc. The regional haze formation in basin areas, along with inte...
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Published in | Atmospheric chemistry and physics Vol. 23; no. 2; pp. 1147 - 1167 |
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Main Authors | , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
23.01.2023
Copernicus Publications |
Subjects | |
Online Access | Get full text |
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Summary: | Haze pollution is a severe environmental problem, caused by elevation of
fine particles (aerodynamic diameter <2.5 µm, PM2.5),
which is related to secondary aerosol formation, unfavourable synoptic
conditions and regional transport, etc. The regional haze formation in basin
areas, along with intensive emission of precursors, high relative humidity
and poor dispersion conditions, is still limitedly understood. In this study,
a field campaign was conducted to investigate the factors resulting in haze
formation in the Sichuan Basin (SCB) during winter in 2021. The fine aerosol
chemical composition was characterised using a time-of-flight aerosol
chemical speciation monitor (ToF-ACSM), which also provided detailed
information on the sources for organic aerosols (OAs). The average
concentration of non-refractory fine particles (NR-PM2.5) was 98.5±38.7 µg m−3, and organics aerosols, nitrate, sulfate,
ammonium and chloride took up 40.3 %, 28.8 %, 10.6 %, 15.3 % and 5.1 % of
PM2.5. Three factors, including a hydrocarbon-like OA (HOA), a biomass
burning OA (BBOA) and an oxygenated OA (OOA), were identified by applying
the positive matrix factorisation (PMF) analysis, and they constituted 24.2 %,
24.2 % and 51.6 % of OA on average, respectively. Nitrate formation was
promoted by gas-phase and aqueous-phase oxidation, while sulfate was mainly
formed through aqueous-phase process. OOA showed strong dependence on Ox,
demonstrating the contribution of photooxidation to OOA formation. OOA
concentration increased as aerosol liquid water content (ALWC) increased
within 200 µg m−3 and kept relatively constant when ALWC
>200 µg m−3, suggesting the insignificant effect of
aqueous-phase reactions on OOA formation. Among the three haze episodes
identified during the whole campaign, the driving factors were different:
the first haze episode (H1) was driven by nitrate formation through
photochemical and aqueous-phase reactions, and the second haze episode (H2)
was mainly driven by the intense emission of primary organic aerosols from
biomass burning and vehicle exhaust, while the third haze episode (H3) was
mainly driven by reactions involving nitrate formation and biomass burning
emission. HOA and BBOA were scavenged, while OOA, nitrate and sulfate
formation was enhanced by aqueous-phase reactions during fog periods, which
resulted in the increase of O:C from pre-fog to post-fog periods. This study
revealed the factors driving severe haze formation in the SCB and implied the
benefit of controlling nitrate as well as intense biomass burning and
vehicle exhaust emission for the mitigation of heavy aerosol pollution in
this region. |
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ISSN: | 1680-7324 1680-7316 1680-7324 |
DOI: | 10.5194/acp-23-1147-2023 |