Title of article :
Optical properties of size-resolved particles at a Hong Kong urban site during winter
Author/Authors :
Gao، نويسنده , , Yuan and Lai، نويسنده , , Senchao and Lee، نويسنده , , Shun-Cheng and Yau، نويسنده , , Pui Shan and Huang، نويسنده , , Yu and Cheng، نويسنده , , Yan and Wang، نويسنده , , Tao and Xu، نويسنده , , Zheng and Yuan، نويسنده , , Chao and Zhang، نويسنده , , Yingyi، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2015
Abstract :
Visibility degradation in Hong Kong is related to the cityʹs serious air pollution problems. To investigate the aerosolsʹ 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 0.056 μm were used to collect size-resolved particle samples. The average Bsp and Bap were 201.96 ± 105.82 Mm− 1 and 39.91 ± 19.16 Mm− 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 (0.56–1.8 μm) 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 (0.56–1.8 μm) and condensation (0.1–0.56 μm) 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.
Keywords :
Size-resolved PM , Aerosol light extinction , Chemical species , source apportionment
Journal title :
Atmospheric Research
Journal title :
Atmospheric Research