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Light absorption coefficient measurement of SOA using a UV–Visible spectrometer connected with an integrating sphere

Authors :
Zhong, Min
Jang, Myoseon
Source :
Atmospheric Environment. Aug2011, Vol. 45 Issue 25, p4263-4271. 9p.
Publication Year :
2011

Abstract

Abstract: A method for measuring an aerosol light absorption coefficient (Ba ) has been developed using a conventional UV–visible spectrometer equipped with an integrating sphere covering a wide range of wavelengths (280–800 nm). The feasibility of the proposed method was evaluated in both the transmittance mode (TUV-IS) and the reflective mode (RUV-IS) using the reference aerosol known for the cross-sectional area. The aerosol was collected on a conventional filter and measured for Ba values. The resulting RUV-IS method was applied to measure light absorption of secondary organic aerosol (SOA). SOA was produced through photooxidation of different precursor hydrocarbons such as toluene, d-limonene and α-pinene in the presence of NOx (60–70 ppb) and inorganic seed aerosol using a 2-m3 indoor Teflon film chamber. Of the three precursor hydrocarbons, the Ba value of toluene SOA (0.574 m2 g−1 at 350 nm) was the highest compared with Ba values for α-pinene SOA (0.029 m2 g−1) and d-limonene SOA (0.038 m2 g−1). When d-limonene SOA or toluene SOA was internally mixed with neutral [(NH4)2SO4] or acidic inorganic seed (NH4HSO4:H2SO4 = 1:1 by mole), the SOA showed 2–3 times greater Ba values at 350 nm than the SOA with no seed. Aerosol aging with a light source for this study reduced Ba values of SOA (e.g., on average 10% for toluene SOA and 30% for d-limonene SOA within 4 h). Overall, weak absorption appeared for chamber-generated SOA over wavelengths ranging from 280 to 550 nm, which fall into the sunlight spectrum. [Copyright &y& Elsevier]

Details

Language :
English
ISSN :
13522310
Volume :
45
Issue :
25
Database :
Academic Search Index
Journal :
Atmospheric Environment
Publication Type :
Academic Journal
Accession number :
61980634
Full Text :
https://doi.org/10.1016/j.atmosenv.2011.04.082