贺兰山地区沙尘气溶胶瞬时谱分析及拟合
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国家自然科学基金资助项目(40365002);南京信息工程大学科研基金资助项目(QD06)


Analysis and Fitting of the Instantaneous Size Distribution of Sand-Dust Aerosol Particles in Helan Mountainous Area
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    摘要:

    利用APS-3310A型激光空气动力学粒子谱仪,1998年4、5月和1999年4月在贺兰山附近的巴音浩特、盐池、银川等地采集了具有代表性的背景大气、浮尘、扬沙、沙尘暴天气条件下沙尘粒子谱分布资料。对粒子瞬时谱的统计分析发现:不同的沙尘天气过程中,气溶胶的瞬时浓度存在很大差别。扬沙、沙尘暴天气过程中,气溶胶浓度变化较大;浮尘天气过程中,气溶胶浓度变化较小。沙尘现象越强,粗粒子(d>
    2.5μm)越多,各粒径段浓度变化越明显。不同过程,粗细粒子对粒子表面积浓度贡献程度不一。沙尘气溶胶粒子谱型为单峰结构,对粒子的瞬时谱进行了谱型拟合,其具有对数正态分布函数的特征。

    Abstract:

    Sand-dust aerosol particle size distributions have been measured by the APS-3310A(made by U.S.A) in Bayinhaote,Yanchi,and Yinchuan nearby the Helan Mountains during the April and May of 1998,and the April of 1999,respectively.A lot of data have been collected under different weather conditions,i.e.background,floating dust,blowing sand,and sand storm.The rules of sand aerosol particle size distribution are found through statistical analysis.Sand aerosol concentration is changeable in different weather processes.During the blowing sand and sand storm weather,aerosol concentration changes a lot,but during the floating dust weather,the circumstance don’t exist.The stronger the aerosol concentration,the more the number of aerosol particles greater than 2.5μm,and the more obvious the change in the concentration of various diameter ranges.During the four processes,coarse and fine particles have different contribution to the surface concentration.The mean instantaneous measured size distributions of sand aerosols are characterized by 1-mode-a single peak mode,which can be fitted very well by a log-normal distribution function.

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顾宇丹,牛生杰,2006.贺兰山地区沙尘气溶胶瞬时谱分析及拟合[J].大气科学学报,29(4):500-506. GU Yu-dan, NUI Sheng-jie,2006. Analysis and Fitting of the Instantaneous Size Distribution of Sand-Dust Aerosol Particles in Helan Mountainous Area[J]. Trans Atmos Sci,29(4):500-506.

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  • 收稿日期:2005-07-21
  • 最后修改日期:2006-03-03
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