Chemical characteristics of aerosol particles (PM2.5) at a site of Horqin Sand-land in northeast China

The objective of this study was to characterize the mass concentration and chemical composition of aerosol particles(PM2.5) collected at Tongliao(Inner Mongolia Autonomous Region, China), a site in Horqin Sand-land in northeast China. During spring 2005, the mass concentration for PM2.5 was (126±71)...

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Veröffentlicht in:Journal of environmental sciences (China) 2006, Vol.18 (4), p.701-707
1. Verfasser: SHEN Zhen-xing CAO Jun-ji LI Xu-xiang WANG Ya-qiang JIE Dong-mei ZHANG Xiao-ye
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Sprache:eng
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Zusammenfassung:The objective of this study was to characterize the mass concentration and chemical composition of aerosol particles(PM2.5) collected at Tongliao(Inner Mongolia Autonomous Region, China), a site in Horqin Sand-land in northeast China. During spring 2005, the mass concentration for PM2.5 was (126±71)μg/m^3 in average. Five dust storm events were monitored with higher concentration of (255 ± 77)μg/m^3 in average than the non dusty days of (106 ± 44)μg/m^3. Concentrations for 20 elements were obtained by the PIXE method. Mass concentrations of ALl, Mg, Si, K, Ca, Ti, Mn, and V, which increased with the PM2.5 concentration, were higher than the pollution elements (S, Cl, Zn, Ar, Se, Br, and Pb). Enrichment factor relative to crust material was also calculated, which showed dust trace elements were mainly from earth upper crust and pollution elements were dominated the anthropogenic aerosols. The Si/Al, Ca/Al, and Fe/Al ratios in PM2.5 samples at Tongliao were 4.07, 0.94, and 0.82, respectively, which were remarkably different with those on other source regions, such as "Western desert source region", "North desert source region" and central Asia source. Air mass back-trajectory analysis identified three kinds of general pathways were associated with the aerosol particle transport to Tongliao, but have the similar elemental ratios, implying that elemental signatures for dust aerosol from Horqin Sand-land were different with other regions.
ISSN:1001-0742
1878-7320