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Aerosol mass spectrometers (AMS) have been widely used for characterization of submicron aerosol (PM 1 ) species in the world. However, the chemical differences between PM 1 and fine particles (PM 2.5 ) in megacities are poorly understood. Here a PM 1 high-resolution AMS with standard vaporizer (SV) and a PM 2.5 time-of-flight aerosol chemical speciation monitor (ToF-ACSM) with capture vaporizer (CV) were deployed simultaneously in summer and winter in Beijing, China, and the chemical differences of non-refractory aerosol species between PM 1 and PM 2.5 were characterized. Our results showed that aerosol species in PM 2.5 were overall highly correlated with those in PM 1 ( r 2 > 0.8), yet the PM 1 /PM 2.5 ratios varied largely for different aerosol species. Nitrate existed dominantly in PM 1 (80–90%), while a considerable fraction of sulfate (30–45%) was observed in the range of 1–2.5 μm (PM 1–2.5 ). Comparatively, PM 1 organics showed higher fractions in PM 2.5 in summer than winter (∼70%). The changes in PM 1 /PM 2.5 ratios of secondary inorganic aerosol (SIA) depended strongly on relative humidity (RH) in summer with considerable decreases as the increase of RH, while such a RH dependence of PM 1 /PM 2.5 ratios was not significant in winter due to the absence of high RH data. We further compared the source apportionment results of organic aerosol (OA) between PM 1 and PM 2.5 . Similar to previous studies, the SV AMS reported ubiquitously higher primary OA than the CV ToF-ACSM, nearly by a factor of 2 for cooking OA, and the difference in secondary OA composition can be substantial, particularly in winter. With the simultaneous measurements of AMS and ACSM, a parameterized relationship between oxygen-to-carbon (O/C) ratio and CV f 44 (fraction of m/z 44 in OA) in summer and winter was developed, which has a potential implication for studying the oxidation and hygroscopicity properties of OA considering the rapid increases in CV ToF-ACSM measurements worldwide.
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Li et al. (2023) studied this question.
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