首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Chemical characterization of ambient aerosol collected during the northeast monsoon season over the Arabian Sea: Labile-Fe(II) and other trace metals - art. no. 4408
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Chemical characterization of ambient aerosol collected during the northeast monsoon season over the Arabian Sea: Labile-Fe(II) and other trace metals - art. no. 4408

机译:在阿拉伯季风的东北季风期间在阿拉伯海收集的环境气溶胶的化学表征:Labile-Fe(II)和其他痕量金属-艺术。没有。 4408

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1] Ambient aerosol samples were collected over the Arabian Sea during the month of March of 1997, aboard the German R/V Sonne, as part of the German Joint Global Ocean Flux Study (JGOFS) project. This is the third study in a series of analogous measurements taken over the Arabian Sea during different seasons of the monsoon. Dichotomous high-volume collector samples were analyzed for ferrous iron immediately after collection, while trace metals, anions, and cations were determined upon return to the laboratory. The main crustal component was geochemically well represented by the average crustal composition and amounted to 5.94 +/- 3.08 mg m(-3). An additional crustal constituent of clay-like character, rich in water-soluble Ca and Mg, was seen in the fine fraction in air masses of Arabian origin. Total ferrous iron concentrations varied from 3.9 to 17.2 ng m(-3) and averaged 9.8 +/- 3.4 ng m(-3), with 87.2% of Fe(II) present in the fine aerosol fraction. Fe(II) concentrations accounted for on average 1.3 +/- 0.5% of the total Fe. While ferrous iron in the coarse fraction appeared to be correlated with the main crustal component, the fine Fe(II) fraction exhibited a more complex behavior. The anthropogenic contribution to the aerosol, as traced by Pb, Zn, and some anions and cations, was found to be considerably larger, especially during the first 10 days of this cruise, than in previously collected samples from the inter-monsoon and southwest monsoon of 1995. [References: 48
机译:1] 1997年3月,作为德国联合全球海洋通量研究(JGOFS)项目的一部分,在德国R / V船上通过阿拉伯海收集了大气气溶胶样品。这是在季风不同季节在阿拉伯海进行的一系列类似测量中的第三项研究。收集后立即对二分类的大体积收集器样品进行二价铁分析,同时返回实验室后测定痕量金属,阴离子和阳离子。平均地壳组成在地球化学上很好地代表了主要地壳成分,其含量为5.94 +/- 3.08 mg m(-3)。在阿拉伯起源的空气中,可以看到细小部分的黏土状地壳成分,富含水溶性的Ca和Mg。总亚铁浓度从3.9到17.2 ng m(-3)不等,平均为9.8 +/- 3.4 ng m(-3),其中87.2%的Fe(II)存在于细小气溶胶级分中。 Fe(II)浓度平均占总Fe的1.3 +/- 0.5%。虽然粗级分中的亚铁似乎与主要地壳成分相关,但细级的Fe(II)级分表现出更复杂的行为。发现Pb,Zn和一些阴离子和阳离子对人为气溶胶的贡献要比以前从季风和西南季风中采集的样本大得多,尤其是在这次航行的前十天1995年。[参考:48

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