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• W3182172868 abstract "Abstract In this study, we investigated the chemical composition and hygroscopicity of water‐soluble fraction in PM 2.5 collected from a rural site of Guanzhong Basin, a highly polluted region in northwest China. We found that inorganic components are the main substances promoting the hygroscopic properties of particulate matter (PH) in summer, while in winter, an increasing contribution from water‐soluble organic matters (WSOM) was observed. The sulfate‐nitrate‐ammonium concentration is higher on heavily polluted days, and a high concentration of water‐soluble organic matter was observed in non‐polluting days. Hygroscopic growth factors, g (RH), with elevated relative humidity (RH) of water‐soluble matter (WSM) were measured for 50, 75, 100, 125, 150 nm by hygroscopic tandem differential mobility analyzer. An initial dry particle diameter of 100 nm was chosen as the research object because the particle size has little effect on the hygroscopic growth factor at RH = 90%. The g (90%) WSM and κ WSM was in the range of 1.19–1.49 and 0.06–0.22 in summer, 1.24–1.49 and 0.08–0.22 in winter, respectively, which is similar to the hygroscopicity parameters of PH produced by biomass burning. The g (90%) WSOM and κ WSOM , obtained using E‐AIM model and Zdanovskii‐Stokes‐Robinson approach, were in the range of 1.06–1.69 and 0.02–0.36 in summer, 1.06–1.58 and 0.02–0.28 in winter, respectively. The hygroscopicity parameters of water‐soluble organic matter is close to the value of levoglucosan, an indicator of biomass burning, implying this region is highly affected by biomass burning. Overall, our results revealed that PM 2.5 in rural regions of Guanzhong Basin is mainly influenced by biomass burning." @default.
• W3182172868 created "2021-07-19" @default.
• W3182172868 creator A5003195401 @default.
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• W3182172868 date "2021-07-26" @default.
• W3182172868 modified "2023-10-14" @default.
• W3182172868 title "Hygroscopicity of Water‐Soluble PM_2.5 in Rural Northwest China: Contrasting Contributors Between Summer and Winter" @default.
• W3182172868 cites W1070066775 @default.
• W3182172868 cites W1250478016 @default.
• W3182172868 cites W1581478352 @default.
• W3182172868 cites W1688467598 @default.
• W3182172868 cites W186296807 @default.
• W3182172868 cites W1921275452 @default.
• W3182172868 cites W1965798812 @default.
• W3182172868 cites W1978806953 @default.
• W3182172868 cites W1983899327 @default.
• W3182172868 cites W1991612968 @default.
• W3182172868 cites W1992751990 @default.
• W3182172868 cites W1994883898 @default.
• W3182172868 cites W1995040519 @default.
• W3182172868 cites W2001324572 @default.
• W3182172868 cites W2003966715 @default.
• W3182172868 cites W2004753519 @default.
• W3182172868 cites W2021872914 @default.
• W3182172868 cites W2032283731 @default.
• W3182172868 cites W2033879042 @default.
• W3182172868 cites W2035618697 @default.
• W3182172868 cites W2039219117 @default.
• W3182172868 cites W2040239281 @default.
• W3182172868 cites W2046239698 @default.
• W3182172868 cites W2047499953 @default.
• W3182172868 cites W2049594613 @default.
• W3182172868 cites W2049903158 @default.
• W3182172868 cites W2053766779 @default.
• W3182172868 cites W2053984466 @default.
• W3182172868 cites W2060899162 @default.
• W3182172868 cites W2064194770 @default.
• W3182172868 cites W2069977802 @default.
• W3182172868 cites W2073340285 @default.
• W3182172868 cites W2081428396 @default.
• W3182172868 cites W2082212766 @default.
• W3182172868 cites W2083441060 @default.
• W3182172868 cites W2085461611 @default.
• W3182172868 cites W2088844241 @default.
• W3182172868 cites W2090142546 @default.
• W3182172868 cites W2096067640 @default.
• W3182172868 cites W2099636727 @default.
• W3182172868 cites W2105463749 @default.
• W3182172868 cites W2115754251 @default.
• W3182172868 cites W2120235685 @default.
• W3182172868 cites W2121994682 @default.
• W3182172868 cites W2122054302 @default.
• W3182172868 cites W2123648333 @default.
• W3182172868 cites W2129566845 @default.
• W3182172868 cites W2129690090 @default.
• W3182172868 cites W2143134463 @default.
• W3182172868 cites W2150751323 @default.
• W3182172868 cites W2153986208 @default.
• W3182172868 cites W2158969163 @default.
• W3182172868 cites W2160915871 @default.
• W3182172868 cites W2164346229 @default.
• W3182172868 cites W2171872502 @default.
• W3182172868 cites W2191459044 @default.
• W3182172868 cites W2233384741 @default.
• W3182172868 cites W2279183079 @default.
• W3182172868 cites W2289415280 @default.
• W3182172868 cites W2305364957 @default.
• W3182172868 cites W2398738719 @default.
• W3182172868 cites W2413842307 @default.
• W3182172868 cites W2509119378 @default.
• W3182172868 cites W2510854028 @default.
• W3182172868 cites W2534298363 @default.
• W3182172868 cites W2551680240 @default.
• W3182172868 cites W2554285426 @default.
• W3182172868 cites W2558295344 @default.
• W3182172868 cites W2607788196 @default.
• W3182172868 cites W2754235196 @default.
• W3182172868 cites W2757572832 @default.
• W3182172868 cites W2781923821 @default.
• W3182172868 cites W2788470671 @default.
• W3182172868 cites W2795406735 @default.
• W3182172868 cites W2802934597 @default.
• W3182172868 cites W2868244763 @default.
• W3182172868 cites W2883485400 @default.
• W3182172868 cites W2892612504 @default.
• W3182172868 cites W2900532783 @default.
• W3182172868 cites W2904080685 @default.
• W3182172868 cites W2911262952 @default.
• W3182172868 cites W2911547802 @default.
• W3182172868 cites W2914376135 @default.
• W3182172868 cites W2942585918 @default.
• W3182172868 cites W2944202717 @default.
• W3182172868 cites W2946996403 @default.

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