Tetragonal CsPbBr nanosheets were obtained by an oriented attachment of orthorhombic CsPbBr nanocubes, involving a lateral shape evolution from octagonal to square. Meanwhile, the experimental results, together with DFT simulation results, indicated that the tetragonal CsPbBr is an indirect bandgap semiconductor that is PL-inactive with a bandgap of 2.979 eV.
Knowledge of the
relative abundance of primary organic aerosol
(POA) and secondary organic aerosol (SOA) forms an important scientific
basis for formulating particulate matter (PM) control policies. Taking
advantage of a comprehensive chemical composition data set of PM2.5 including both POA and SOA tracers (most notably, SOA tracers
of a few biogenic voltaic organic compound precursors), we investigate
the impact of inclusion of SOA tracers on the source apportionment
of organic carbon (OC) and PM2.5 in the Pearl River Delta
region of China using positive matrix factorization (PMF). In PMF
runs incorporating SOA tracers (PMFw), ten PMF factors
were resolved including four secondary factors: (1) SOA I (α-pinene,
β-caryophyllene, and naphthalene-derived SOA), (2) SOA II (isoprene-derived
SOA), (3) a secondary sulfate factor, and (4) a secondary nitrate
factor. In PMF tests without SOA tracers (PMFwo), the SOA
I and SOA II factors could not be extracted, but the remaining eight
source factors were resolved. Among the eight common source factors,
the industrial emission factor, identified by high loadings of Zn
and Pb, showed the largest variations between PMFw and
PMFwo solutions. The source contributions of SOA I and
SOA II resolved in PMFw were largely shifted to the industry
emission source in PMFwo. Secondary organic carbon (SOC)
summed from the four secondary factors in PMFw contributed
∼40% (4.47 μgC/m3), and the SOC estimate by
PMFwo (3.51 μgC/m3) was 21% lower due
to the inability to extract SOA I and SOA II. Secondary PM2.5 by PMFwo was 6% lower than that by PMFw (23.7
vs 25.2 μg/m3). The PMFw results indicated
that SOC from specific precursors may have different formation pathways
than secondary sulfate and nitrate formation processes, and their
source contributions could not be properly resolved without the indicative
tracers included in PMF. This study demonstrates the utility of biogenic
SOA tracers in resolving isoprene-derived SOA and highlights the need
for more SOA tracers, especially those specific to anthropogenic precursors,
in improving the source apportionment for those broad OA sources such
as industrial emissions.
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