Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, China.
Environ Pollut. 2010 Nov;158(11):3392-400. doi: 10.1016/j.envpol.2010.07.036.
Carbonaceous aerosols were studied at three background sites in south and southwest China. Hok Tsui in Hong Kong had the highest concentrations of carbonaceous aerosols (OC=8.7±4.5μg/m(3), EC=2.5±1.9μg/m(3)) among the three sites, and Jianfeng Mountains in Hainan Island (OC=5.8±2.6μg/m(3), EC=0.8±0.4μg/m(3)) and Tengchong mountain over the east edge of the Tibetan Plateau (OC=4.8±4.0μg/m(3), EC=0.5±0.4μg/m(3)) showed similar concentration levels. Distinct seasonal patterns with higher concentrations during the winter, and lower concentrations during the summertime were observed, which may be caused by the changes of the regional emissions, and monsoon effects. The industrial and vehicular emissions in East, Southeast and South China, and the regional open biomass burning in the Indo-Myanmar region of Asia were probably the two major potential sources for carbonaceous matters in this region.
在中国南方和西南部的三个背景站点研究了含碳气溶胶。三个站点中,香港鹤咀的含碳气溶胶浓度最高(OC=8.7±4.5μg/m³,EC=2.5±1.9μg/m³),而海南岛尖峰岭(OC=5.8±2.6μg/m³,EC=0.8±0.4μg/m³)和青藏高原东缘的腾冲山(OC=4.8±4.0μg/m³,EC=0.5±0.4μg/m³)的浓度水平相似。观测到明显的季节性变化,冬季浓度较高,夏季浓度较低,这可能是由于区域排放和季风的变化所致。东亚、东南亚和华南的工业和车辆排放,以及亚洲印度-缅甸地区的区域开放生物质燃烧,可能是该地区含碳物质的两个主要潜在来源。