TY - JOUR
T1 - Optical properties of size-resolved particles at a Hong Kong urban site during winter
AU - Gao, Yuan
AU - Lai, Senchao
AU - Lee, Shuncheng
AU - Yau, Pui Shan
AU - Huang, Yu
AU - Cheng, Yan
AU - Wang, Tao
AU - Xu, Zheng
AU - Yuan, Chao
AU - Zhang, Yingyi
PY - 2015/3/5
Y1 - 2015/3/5
N2 - Visibility degradation in Hong Kong is related to the city's serious air pollution problems. To investigate the aerosols' optical properties and their relationship with the chemical composition and size distribution of the particles, a monitoring campaign was conducted at an urban site in the early winter period (from October to December, 2010). The particle light scattering coefficient (Bsp) and absorption coefficient (Bap) were measured. Two collocated Micro-Orifice Uniform Deposit Impactor samplers (MOUDI110, MSP, USA) with nominal 50% cut-off aerodynamic diameters of 18, 10, 5.6, 3.2, 1.8, 1, 0.56, 0.32, 0.18, 0.1, and 0.056μm were used to collect size-resolved particle samples. The average Bspand Bapwere 201.96±105.82Mm-1and 39.91±19.16Mm-1, with an average single scattering albedo (ωo) of 0.82±0.07. The theoretical method of light extinction calculation was used to determine the extinction of the size-resolved particulate matters (PM). The reconstructed light scattering coefficient correlated well with the measured scattering value in the Hong Kong urban area. Droplet mode (0.56-1.8μm) particles contributed most to the particle light extinction (~69%). Organic matter, ammonium sulphate and elemental carbon were the key components causing visibility degradation in the droplet (0.56-1.8μm) and condensation (0.1-0.56μm) size ranges. Five sources contributing to particle light extinction have been identified using positive matrix factorisation (PMF). Traffic/engine exhausts and secondary aerosols accounted for ~36% and ~32% of particle light extinction, respectively, followed by sea salt (15%). The remaining sources, soil/fugitive dust and tire dust, contributed by ~10% and 7%, respectively, to particle light extinction.
AB - Visibility degradation in Hong Kong is related to the city's serious air pollution problems. To investigate the aerosols' optical properties and their relationship with the chemical composition and size distribution of the particles, a monitoring campaign was conducted at an urban site in the early winter period (from October to December, 2010). The particle light scattering coefficient (Bsp) and absorption coefficient (Bap) were measured. Two collocated Micro-Orifice Uniform Deposit Impactor samplers (MOUDI110, MSP, USA) with nominal 50% cut-off aerodynamic diameters of 18, 10, 5.6, 3.2, 1.8, 1, 0.56, 0.32, 0.18, 0.1, and 0.056μm were used to collect size-resolved particle samples. The average Bspand Bapwere 201.96±105.82Mm-1and 39.91±19.16Mm-1, with an average single scattering albedo (ωo) of 0.82±0.07. The theoretical method of light extinction calculation was used to determine the extinction of the size-resolved particulate matters (PM). The reconstructed light scattering coefficient correlated well with the measured scattering value in the Hong Kong urban area. Droplet mode (0.56-1.8μm) particles contributed most to the particle light extinction (~69%). Organic matter, ammonium sulphate and elemental carbon were the key components causing visibility degradation in the droplet (0.56-1.8μm) and condensation (0.1-0.56μm) size ranges. Five sources contributing to particle light extinction have been identified using positive matrix factorisation (PMF). Traffic/engine exhausts and secondary aerosols accounted for ~36% and ~32% of particle light extinction, respectively, followed by sea salt (15%). The remaining sources, soil/fugitive dust and tire dust, contributed by ~10% and 7%, respectively, to particle light extinction.
KW - Aerosol light extinction
KW - Chemical species
KW - Size-resolved PM
KW - Source apportionment
UR - http://www.scopus.com/inward/record.url?scp=84916937776&partnerID=8YFLogxK
U2 - 10.1016/j.atmosres.2014.10.020
DO - 10.1016/j.atmosres.2014.10.020
M3 - Journal article
SN - 0169-8095
VL - 155
SP - 1
EP - 12
JO - Atmospheric Research
JF - Atmospheric Research
ER -