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Characterization of fine particulate black carbon in Guangzhou, a megacity of South China

机译:中国南方大城市广州的细颗粒黑炭的表征

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Continuous measurement of fine particulate black carbon (BC) was conducted at an urban site of Guangzhou in South China from December 2007 to December 2008. The daily average BC concentrations ranged from 0.6 to 20.5 μg m−3, with an average value of 4.7 μg m−3, which was substantially higher than those observed in the urban areas of other developed countries. Diurnal fluctuations of BC were marked with two peaks, one in the morning rush hour (08:00 LT) and the other in the late evening hour (21:00–22:00 LT), while the lowest BC concentrations were observed in the afternoon. Ambient BC concentrations displayed significant seasonal and diurnal variations with higher values in winter and spring, followed by lower concentrations during autumn and summer. Wind speed, wind direction and temperature were important meteorological factors that affected BC concentrations. A clearly negative correlation (r = −0.50, p  0.01) between BC concentrations and wind speed was found during the study period. A specific investigation was conducted to determine the relationship between optical BC and thermal–optical–reflectance elemental carbon (TOR EC) in distinct seasons. Although significant correlations between BC and EC were obtained (r  0.92, p  0.01), the regression slopes (ΔBC/ΔEC) slightly deviated from each other with values of 0.79, 1.18, and 0.81 in winter, spring and summer, respectively, possibly due to the distinct mixing states and source variations in different seasons. The calculated experimental attenuation coefficient showed a higher value (19.3 m2 g−1) in Guangzhou than the one recommended for typical Aethalometer measurements.
机译:从2007年12月至2008年12月,在华南广州市区进行了细颗粒黑碳(BC)的连续测量。日平均BC浓度范围为0.6至20.5μgm -3 ,平均值为4.7μgm −3 ,大大高于其他发达国家市区的平均值。 BC的昼夜波动有两个峰值,一个是在高峰时间(08:00 LT),另一个是在傍晚时间(21:00-22:00 LT),而BC的最低浓度在下午。环境中的BC浓度显示出明显的季节和昼夜变化,冬季和春季具有较高的值,秋季和夏季则具有较低的浓度。风速,风向和温度是影响BC浓度的重要气象因素。研究期间发现BC浓度与风速之间存在明显的负相关( r = − 0.50, p <0.01)。进行了一项专门调查,以确定不同季节的光学BC与热-光学-反射元素碳(TOR EC)之间的关系。尽管获得了BC和EC之间的显着相关性( r p <0.01),但回归斜率(ΔBC/ΔEC)彼此略有偏离,值为0.79分别在冬季,春季和夏季分别为1.18和0.81,这可能是由于不同季节的明显混合状态和来源变化所致。计算出的实验衰减系数在广州显示出比典型的湿度计测量推荐的值更高的值(19.3m 2 g -1 )。

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