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Secondary Organic Material Produced by the Dark Ozonolysis of α-Pinene Minimally Affects the Deliquescence and Efflorescence of Ammonium Sulfate

机译:由α-Material烯的黑暗臭氧分解产生的次要有机材料最小地影响硫酸铵的潮解和风化。

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摘要

The hygroscopic phase transitions and growth factors of mixed particles having as components ammonium sulfate and secondary organic material (SOM) were measured. The SOM was generated by the dark ozonolysis of α-pinene, and organic particle mass concentrations of 1.63 and 12.2 μg m−3 were studied. The hygroscopic properties were investigated using a 1×3 tandem differential mobility analyzer (1×3-TDMA). The 1×3-TDMA takes advantage of the hysteresis between solid-to-aqueous and aqueous-to-solid phase transitions to determine the efflorescence and deliquescence relative humidities (ERH and DRH, respectively) of materials. Overall, the influence of the SOM produced by the dark ozonolysis of α-pinene on the ERH and DRH of ammonium sulfate was small, shifting for example the DRH from 80% for pure ammonium sulfate to 77% for organic volume fractions of 0.96. The ERH likewise shifted by only a small amount across this composition range, specifically from 31 to 29%. The SOM produced at the lower organic particle mass concentrations shifted ERH and DRH even less, indicating an influence of SOM chemical composition on phase transitions. The hygroscopic growth factors of the mixed particles were adequately modeled across the range of studied RH (50 to 83%) using volume-averaged growth factors of the pure materials. The results for ERH, DRH, and the growth factors were all consistent with a model of phase separation between the inorganic and organic phases in individual particles, at least for the studied RH values (<83%) and for SOM prepared by α-pinene ozonolysis.
机译:测量了具有硫酸铵和第二有机材料(SOM)作为成分的混合颗粒的吸湿性相变和生长因子。 SOM是由α-pine烯的黑暗臭氧分解产生的,并且研​​究了有机粒子质量浓度为1.63和12.2μgm ˆ3 。使用1×3串联差动迁移率分析仪(1×3-TDMA)研究了吸湿性。 1 3-TDMA利用固-水相和水-固相变之间的滞后来确定材料的风化和潮解相对湿度(分别为ERH和DRH)。总体而言,由α-pine烯的黑暗臭氧分解产生的SOM对硫酸铵的ERH和DRH的影响很小,例如DRH从纯硫酸铵的80%变为有机体积分数为0.96的77%。在该组成范围内,ERH同样仅发生了少量变化,具体而言为31%至29%。在较低有机颗粒质量浓度下产生的SOM对ERH和DRH的移动甚至更少,表明SOM化学成分对相变的影响。使用纯材料的体积平均生长因子,可以在研究的相对湿度(50%至83%)的范围内对混合颗粒的吸湿生长因子进行充分建模。 ERH,DRH和生长因子的结果均与单个颗粒的无机相和有机相之间的相分离模型一致,至少对于研究的RH值(<83%)和由S- ene烯臭氧分解。

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  • 来源
    《Aerosol Science and Technology》 |2011年第2期|p.244-261|共18页
  • 作者单位

    School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USA Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 00:57:38

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