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Taiwan Association for Aerosol Research, Aerosol and Air Quality Research, 3(10), p. 255-264, 2010

DOI: 10.4209/aaqr.2009.12.0076

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Hygroscopicity of Inorganic Aerosols: Size and Relative Humidity Effects on the Growth Factor

Journal article published in 2010 by Liping Qiao, Dawei Hu, Jianmin Chen, Xingnan Ye, Xin Yang ORCID, Tiantao Cheng, Wen Fang
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

The hygroscopic properties of inorganic salt particles, including (NH 4) 2 SO 4 , NaCl, Na 2 SO 4 and NaNO 3 , are investigated using a self-assembled hygroscopic tandem differential mobility analyzer (H-TDMA) system. The iso-GF (growth factor) curves are derived to illustrate the effects of the initial particle size (D 0) and relative humidity (RH) on the GFs. For those salt particles of 100 nm, the GFs measured agreed well with their theoretical Köhler curves. In the size range of 20–200 nm, the GFs of (NH 4) 2 SO 4 , NaCl and Na 2 SO 4 particles all continuously decrease with D 0 increasing below the deliquescence RH (DRH). However, when RH is higher than the DRH, the GFs of those salts aerosols increase with D 0 throughout the investigated size range. Similar increase trend of GFs with D 0 is also observed for NaNO 3 aerosols though they do not exhibit the abrupt deliquescence behavior. From iso-GF curves, it can be clearly observed that the GFs of (NH 4) 2 SO4, NaCl and Na 2 SO 4 particles all increase with the RH while the values decrease with D 0 below DRH. And above DRH, the GFs are more sensitive to D 0 for particles smaller than 60 nm, while the GFs are more sensitive to RH for particles larger than 80 nm. For NaNO 3 aerosols, the iso-GF curves indicate the size-effect becomes more prominent on their hygroscopicity as the RH increases. The iso-GF curves provide a lucid and explicit insight into the hygroscopic growth of salts particles. Through iso-GF curves, we can clearly elucidate the major factor that affects the ultimate particle diameter at ambient atmosphere.