中亚沙尘暴气溶胶与其他地区土壤沙尘特征的比较

Laurent Gomes , Dale A. Gillette
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引用次数: 101

摘要

1989年9月在塔吉克斯坦(苏联中亚)收集了沙尘暴气溶胶样本,作为苏联-美国联合尘埃实验的一部分。并与其他地区土壤源性粉尘的物理化学特征进行了比较。颗粒质量-尺寸分布在1 ~ 10 μm之间表现为对数正态分布。样品的化学成分表明,粉尘的钙和硅含量特别丰富,铁含量很低。对粉尘矿物组成的估计表明,苏联亚洲粉尘中Ca和Si的富集一定与碳酸盐和石英的高含量有关。不同的铁/铝也表明了亚洲尘埃中粘土矿物的特定化学成分。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A comparison of characteristics of aerosol from dust storms in Central Asia with soil-derived dust from other regions

Aerosol samples from dust storms were collected in Tadzhikistan (Soviet Central Asia) during September 1989, as a part of the joint U.S.S.R.-U.S. Dust Experiment. Physico-chemical characteristics of deposited dust were compared with those of soil-derived dust collected in other regions. Particle mass-size distributions appear to be characterized by a common log-normal mode between 1 and 10 μm. Chemical composition of the sampled material shows that the dust is particularly rich in calcium and silicon and poor in iron. Estimated mineral composition of dust indicates that this enrichment in Ca and Si for the Soviet Asian dust must be related to high contents of carbonate and quartz, respectively. Different Fe/Al also suggest a specific chemical composition for clay minerals in the Asian dust.

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