4.5 Article

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

Journal

AEROSOL AND AIR QUALITY RESEARCH
Volume 10, Issue 3, Pages 255-264

Publisher

TAIWAN ASSOC AEROSOL RES-TAAR
DOI: 10.4209/aaqr.2009.12.0076

Keywords

H-TDMA; Hygroscopicity; Inorganic aerosols; Size-effect; Iso-GF

Funding

  1. National Natural Science Foundation of China [40575073, 40533017, 40605001, 40728006, 40775080, 40875053]
  2. National Key Technology RD program [2006BAC12B001]
  3. Chinese Ministry of Education [108050]
  4. Science and Technology Commission of Shanghai Municipality [09160707700]

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The hygroscopic properties of inorganic salt particles, including (NH4)(2)SO4, NaCl, Na2SO4 and NaNO3, 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 Kohler curves. In the size range of 20-200 nm, the GFs of (NH4)(2)SO4, NaCl and Na2SO4 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 NaNO3 aerosols though they do not exhibit the abrupt deliquescence behavior. From iso-GF curves, it can be clearly observed that the GFs of (NH4)(2)SO4, NaCl and Na2SO4 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 NaNO3 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.

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