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Mixture state of individual Asian dust particles at a coastal site of Qingdao, China

机译:中国青岛沿海地区亚洲单个尘埃颗粒的混合状态

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In order to investigate the characteristics of Asian dust particles before they leave the continent, particles were collected at a coastal site of Qingdao (120°7′E, 36°6′N) in northeastern China during three dust storm events in spring 2001. The elemental composition and size of individual dust particles, and their mixture state with sea salt, sulfate and nitrate were analyzed using electron microscopes and an energy dispersive spectrometer. It was found that far less than 10% of dust particles were internally mixed with sea salt. Although a number of dust particles contained Na, S, and Cl, the elements in most of the particles were more likely from crustal origins. The combination of reagent tests and elemental analysis revealed that 3.3-12.2% of dust particles contained sulfate and 6.5-10.0% contained nitrate on their surface. Number-size distributions of dust particles estimated from their electron microscope images had a distribution mode of around 3 μm diameter with the range of 1.0-8.0 μm. Out of this range, dust particles were rarely detected.
机译:为了调查亚洲尘埃颗粒离开大陆之前的特征,在2001年春季的三场沙尘暴事件中,在中国东北部青岛的一个沿海地点(120°7′E,36°6′N)收集了这些尘埃。使用电子显微镜和能量色散光谱仪分析了各个尘埃颗粒的元素组成和大小,以及它们与海盐,硫酸盐和硝酸盐的混合状态。据发现,内部只有不到10%的尘埃颗粒与海盐混合。尽管许多尘埃颗粒包含Na,S和Cl,但大多数颗粒中的元素更有可能来自地壳。试剂测试和元素分析的结合显示,其表面的灰尘颗粒中有3.3-12.2%含有硫酸盐,而6.5-10.0%含有硝酸盐。从电子显微镜图像估计的尘埃粒子的数量分布具有直径为3μm的分布模式,范围为1.0-8.0μm。超出此范围,很少检测到灰尘颗粒。

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