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      Field characterization of the PM<sub>2.5</sub> Aerosol Chemical Speciation Monitor: insights into the composition, sources, and processes of fine particles in eastern China

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          Abstract

          <p><strong>Abstract.</strong> A PM<sub>2.5</sub>-capable aerosol chemical speciation monitor (Q-ACSM) was deployed in urban Nanjing, China, for the first time to measure in situ non-refractory fine particle (NR-PM<sub>2.5</sub>) composition from 20 October to 19 November 2015, along with parallel measurements of submicron aerosol (PM<sub>1</sub>) species by a standard Q-ACSM. Our results show that the NR-PM<sub>2.5</sub> species (organics, sulfate, nitrate, and ammonium) measured by the PM<sub>2.5</sub>-Q-ACSM are highly correlated (<i>r</i><sup>2</sup> &amp;gt; 0.9) with those measured by a Sunset Lab OC<span class="thinspace"></span><span class="thinspace"></span>/<span class="thinspace"></span><span class="thinspace"></span>EC analyzer and a Monitor for AeRosols and GAses (MARGA). The comparisons between the two Q-ACSMs illustrated similar temporal variations in all NR species between PM<sub>1</sub> and PM<sub>2.5</sub>, yet substantial mass fractions of aerosol species were observed in the size range of 1–2.5<span class="thinspace"></span>µm. On average, NR-PM<sub>1−2.5</sub> contributed 53<span class="thinspace"></span>% of the total NR-PM<sub>2.5</sub>, with sulfate and secondary organic aerosols (SOAs) being the two largest contributors (26 and 27<span class="thinspace"></span>%, respectively). Positive matrix factorization of organic aerosol showed similar temporal variations in both primary and secondary OAs between PM<sub>1</sub> and PM<sub>2.5</sub>, although the mass spectra were slightly different due to more thermal decomposition on the capture vaporizer of the PM<sub>2.5</sub>-Q-ACSM. We observed an enhancement of SOA under high relative humidity conditions, which is associated with simultaneous increases in aerosol pH, gas-phase species (NO<sub>2</sub>, SO<sub>2</sub>, and NH<sub>3</sub>) concentrations and aerosol water content driven by secondary inorganic aerosols. These results likely indicate an enhanced reactive uptake of SOA precursors upon aqueous particles. Therefore, reducing anthropogenic NO<sub><i>x</i></sub>, SO<sub>2</sub>, and NH<sub>3</sub> emissions might not only reduce secondary inorganic aerosols but also the SOA burden during haze episodes in China.</p>

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          Organic aerosol (OA) particles affect climate forcing and human health, but their sources and evolution remain poorly characterized. We present a unifying model framework describing the atmospheric evolution of OA that is constrained by high-time-resolution measurements of its composition, volatility, and oxidation state. OA and OA precursor gases evolve by becoming increasingly oxidized, less volatile, and more hygroscopic, leading to the formation of oxygenated organic aerosol (OOA), with concentrations comparable to those of sulfate aerosol throughout the Northern Hemisphere. Our model framework captures the dynamic aging behavior observed in both the atmosphere and laboratory: It can serve as a basis for improving parameterizations in regional and global models.
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              Chemical and microphysical characterization of ambient aerosols with the aerodyne aerosol mass spectrometer.

              The application of mass spectrometric techniques to the real-time measurement and characterization of aerosols represents a significant advance in the field of atmospheric science. This review focuses on the aerosol mass spectrometer (AMS), an instrument designed and developed at Aerodyne Research, Inc. (ARI) that is the most widely used thermal vaporization AMS. The AMS uses aerodynamic lens inlet technology together with thermal vaporization and electron-impact mass spectrometry to measure the real-time non-refractory (NR) chemical speciation and mass loading as a function of particle size of fine aerosol particles with aerodynamic diameters between approximately 50 and 1,000 nm. The original AMS utilizes a quadrupole mass spectrometer (Q) with electron impact (EI) ionization and produces ensemble average data of particle properties. Later versions employ time-of-flight (ToF) mass spectrometers and can produce full mass spectral data for single particles. This manuscript presents a detailed discussion of the strengths and limitations of the AMS measurement approach and reviews how the measurements are used to characterize particle properties. Results from selected laboratory experiments and field measurement campaigns are also presented to highlight the different applications of this instrument. Recent instrumental developments, such as the incorporation of softer ionization techniques (vacuum ultraviolet (VUV) photo-ionization, Li+ ion, and electron attachment) and high-resolution ToF mass spectrometers, that yield more detailed information about the organic aerosol component are also described. (c) 2007 Wiley Periodicals, Inc.
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                Author and article information

                Journal
                Atmospheric Chemistry and Physics
                Atmos. Chem. Phys.
                Copernicus GmbH
                1680-7324
                2017
                December 06 2017
                : 17
                : 23
                : 14501-14517
                Article
                10.5194/acp-17-14501-2017
                4d84ffd3-6637-4fad-b782-7c273437f8ae
                © 2017

                https://creativecommons.org/licenses/by/3.0/

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