Chemical characterization of roadside PM2.5 and black carbon in Macao during a summer campaign

被引:22
作者
Song, Shaojie [1 ,2 ]
Wu, Ye [1 ,2 ,3 ]
Zheng, Xuan [1 ,2 ]
Wang, Zhishi [4 ]
Yang, Liu [5 ]
Li, Jiaqi [1 ,2 ]
Hao, Jiming [1 ,2 ,3 ]
机构
[1] Tsinghua Univ, Sch Environm, Beijing 100084, Peoples R China
[2] Tsinghua Univ, State Key Joint Lab Environm Simulat & Pollut Con, Beijing 100084, Peoples R China
[3] State Environm Protect Key Lab Sources & Control, Beijing 100084, Peoples R China
[4] Univ Macau, Fac Sci & Technol, Macau, Peoples R China
[5] Transport Planning & Res Inst, Div Environm & Resources Res, Beijing 100028, Peoples R China
基金
中国国家自然科学基金;
关键词
Fine particulate matter; vehicle emission; chemical composition; size distribution; AIRBORNE PARTICULATE MATTER; SIZE DISTRIBUTIONS; TEMPORAL VARIATIONS; ELEMENTAL CARBON; MAJOR HIGHWAY; URBAN; PM10; PARTICLES; LOCATIONS; GUANGZHOU;
D O I
10.5094/APR.2014.044
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Air pollution is the leading environmental concern in Macao. The temporal variations of particulate matter (PM) and black carbon (BC) mass concentrations and the size-resolved PM2.5 chemical compositions, including trace elements and carbonaceous species, were measured in Macao during a near-road summer campaign. The average concentrations for PM10, PM2.5 and BC at a roadside measurement site were 37.8 mu g m(-3), 31.4 mu g m(-3) and 5.6 mu g m(-3), respectively. Results showed that local emissions contributed at least 35% to PM2.5 mass in Macao. Higher BC concentrations were observed in the daytime than at night, consistent with the diurnal variations of traffic flow. Factor analysis classified trace elements into three categories, representing crustal sources (Mg, Si, Al, Na, Fe, Ca and K), road traffic sources (Cu and Co) and secondary inorganic particle formation (S). Crustal elements and road traffic elements were enriched in the size ranges of >1.0 mu m and <0.2 mu m, respectively. The unimodal distribution pattern with a peak at <0.2 mu m for organic carbon (OC) was probably due to secondary organic aerosol formation, whereas about 70% of elemental carbon (EC) was in the size range of 0.2-1.0 mu m. Secondary organic aerosols were found to be a strong contributor to PM in the size ranges of <0.2 mu m and 1.0-2.5 mu m.
引用
收藏
页码:381 / 387
页数:7
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