新疆和田市沙尘气溶胶浓度及粒径分布特征研究

Study on Concentration and Pariticle Size Distribution Characteristics of Dust Aerosol in Hetian, Xinjiang

  • 摘要: 沙尘气溶胶不仅影响天气和气候,而且对海洋生态及全球物质循环具有重要的作用。塔克拉玛干沙漠作为我国和东亚地区重要的沙尘气溶胶源区,其西南缘和田市沙尘气溶胶浓度及粒径分布特征尚不明确,将不利于该区域沙尘气溶胶远距离输送和沉降的机理研究。因此,本文利用粒子分级采样仪,通过对和田市不同天气(晴天、浮尘、扬沙天气)下沙尘气溶胶浓度及粒径分布特征的研究,得到以下结论: 1)晴天,0.1~2.5 μm、2.5~10 μm、10~20 μm的沙尘气溶胶浓度平均为2612、1059.3、126 μg/m3,分别占68.8%、27.9%、3.3%;浮尘天气,0.1~2.5 μm、2.5~10 μm、10~20 μm的沙尘气溶胶浓度平均为6273、1403、139 μg/m3,分别占79.6%、17.8%、2.5%;扬沙天气,0.1~2.5 μm、2.5~10 μm、10~20 μm的沙尘气溶胶浓度平均为7135、2108、315 μg/m3,分别占74.6%、22%、3.3%。2)晴天、浮尘、扬沙天气0.1~2.5 μm、2.5~10 μm的沙尘气溶胶浓度夜间均高于白天; 10~20 μm的沙尘气溶胶浓度仅在晴天时夜间高于白天,浮尘和扬沙天气则是白天高于夜间。

     

    Abstract: Dust aerosols not only affect weather and climate, but also play an important role in marine ecology and global material circulation. The Taklimakan Desert is an important source of dust aerosols in my country and East Asia. The concentration and particle size distribution characteristics of dust aerosols in the southwestern margin of Hotan City are still unclear, which is not conducive to the study of the mechanism of dust aerosol transport and deposition in this region. Therefore, this paper uses the particle classification sampler to study the characteristics of the dust aerosol concentration and particle size distribution under different weather (sunny, floating dust, blowing sand) in Hotan City, and the following conclusions are obtained: (1) On sunny days, the average dust aerosol concentrations of 0.1-2.5 μm, 2.5-10 μm, and 10-20 μm are 2612, 1059.3, and 126 μg/m3, accounting for 68.8%, 27.9%, and 3.3% respectively; floating dust, the average dust aerosol concentrations of 0.1-2.5 μm, 2.5-10 μm, and 10-20 μm are 6273, 1403, and 139 μg/m3, accounting for 79.6%, 17.8%, and 2.5% respectively; blowing sand, the average dust aerosol concentrations of 0.1-2.5 μm, 2.5-10 μm, and 10-20 μm are 7135, 2108, and 315 μg/m3, accounting for 74.6%, 22%, and 3.3% respectively. (2) In Sunny days, floating dust and blowing sand weather, the concentrations of dust aerosol of 0.1-2.5 μm and 2.5-10 μm at night were higher than those in the daytime. The concentration of dust aerosol of 10-20 μm was higher than that of daytime only in sunny days, while that of floating dust and sand-blowing was higher than that of nighttime.

     

/

返回文章
返回