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成都春季生物质燃烧和沙尘期间气溶胶散射特征及其重建
摘要点击 4954  全文点击 1832  投稿时间:2011-09-04  修订日期:2011-10-20
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中文关键词  PM2.5  生物质燃烧  沙尘  散射系数  重建  贡献因子
英文关键词  PM2.5 aerosol  biomass burning(BB)  dust storm  scattering coefficient  reconstruction  contribution factors
作者单位E-mail
岳建华 环境保护部华南环境科学研究所, 广州 510655 yuejianhua@scies.org 
陶俊 环境保护部华南环境科学研究所, 广州 510655 taojun@scies.org 
林泽健 环境保护部华南环境科学研究所, 广州 510655  
朱李华 环境保护部华南环境科学研究所, 广州 510655  
曹军骥 中国科学院地球环境研究所, 西安 710075  
罗磊 中国气象局成都高原气象研究所, 成都 610071  
中文摘要
      于2009年4月19日~5月17日在成都城区每天采集PM2.5样品. 利用热光碳分析仪、离子色谱、X荧光光谱仪和高效阴离子交换色谱分别分析样品中有机碳/元素碳、水溶性离子、地壳元素和左旋葡聚糖,同步测量了大气散射系数(bsp)和气象数据. 利用IMPROVE方程重建大气散射系数,并与实测大气散射系数进行对比.结果发现,PM2.5浓度均值为133.2 μg·m-3,大气散射系数为530 Mm-1. 左旋葡聚糖和地壳元素能很好地反映生物质燃烧和沙尘事件. 观测期间成都城区计算值bsp'为504 Mm-1,(NH4)2SO4、NH4NO3、OM(organic matter)、FS(fine soil)和CM(coarse mass)贡献率分别为26%、 15%、 53%、 4%和2%. DS(dust storm)期间,计算值bsp'为575 Mm-1,FS和CM贡献率达到17%和21%.BB(biomass burning)期间,计算值bsp'为635 Mm-1,OM贡献率达到62%.
英文摘要
      Aerosol samples for PM2.5 were collected from 19 April to 17 May in 2009 at Chengdu. The concentrations of organic carbon, element carbon, water-solubility ions, crustal elements and levoglucosan of all particle samples were determined by thermal/optical carbon analyzer,ion chromatography, X-ray fluorescence spectrometer and high performance anion exchange chromatography, respectively. In-situ scattering coefficients (bsp) and meteorological parameters for this period were also conducted. Ambient scattering coefficients were reconstructed by IMPROVE formula and compared with measured scattering coefficients. The results showed that the average mass concentration of PM2.5 and measured bsp were 133.2 μg·m-3 and 530 Mm-1, respectively. Levoglucosan and crustal elements were good traces for biomass burning and dust storm events, respectively. The calculated bsp' was 504 Mm-1 during campaigning period. The major contributors to scattering coefficients included: (NH4)2SO4 (26%), NH4NO3 (15%), OM (53%), FS (4%) and CM (2%), respectively. The calculated bsp' was 575 Mm-1 and the dominant species were FS (17%) and CM (21%) during dust storm period (DS). The calculated bsp' was 635 Mm-1 and OM contributed 62% during biomass burning (BB) period.

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