Atmospheric aluminum from human activities

Yoshikazu Hashimoto, Yoshika Sekine, Tsunehiko Otoshi
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引用次数: 26

Abstract

The inventory of aluminum in the atmospheric air from human activities was discussed using data from the Japanese National Air Surveillance Network. The source of atmospheric Al is considered to be mainly soil-derived particles. However, an hropogenically generated Al could also be added to airborne particulates less than 10 μm in aerodynamic diameter. Scandium, which is also found in soil dust, has a value lower than unity in enrichment factor normalized by Al. The intercept, A of the AlSc regression curve, (Al) = A + B(Sc), was much larger in industrial cities such as Kawasaki, Amagasaki, etc. This could be explained by the difference of elemental composition of various emission sources and the existence of excess Al added to airborne particulate samples.

大气中的铝来源于人类活动
利用日本国家空气监测网的数据,讨论了人类活动造成的大气中铝的库存。大气中铝的主要来源被认为是来自土壤的颗粒。然而,人工生成的Al也可以添加到空气动力学直径小于10 μm的空气颗粒中。土壤粉尘中钪的富集系数经Al归一化后小于1。AlSc回归曲线(Al) = a + B(Sc)的截距a在川崎、天崎等工业城市要大得多。这可以解释为各种排放源元素组成的差异以及大气颗粒物样品中存在过量的Al。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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