Kamani Hossein, Hoseini Mohammad, Safari Gholam Hossein, Jaafari Jalil, Mahvi Amir Hossein
Health Promotion Research Center, Zahedan University of Medical Sciences, Zahedan, Iran.
Environ Monit Assess. 2014 Aug;186(8):5059-67. doi: 10.1007/s10661-014-3759-9. Epub 2014 Apr 10.
In this study, measurements of the trace metals Zn, Cd, Cr, Ni, Pb, Cu, Fe and Al were performed on 53 wet atmospheric precipitation samples (snow and rainwater) collected at a central site of Tehran. Samples were collected using a bulk sampler equipped with a high-density polyethylene funnel from November to May in 2011 and 2012 on the roof of a building in the city centre. Trace metals in the filtered samples were measured with ICP-MS. Statistical analysis of the results revealed that Al, which is principally a crustal-derived element, was the highest mean measured concentration. The pH ranged from 4.2 to 7.1 with a mean value of 5.1. Crustal enrichment factors (EFc) related to the relative abundance of elements in crustal material was calculated using Al as reference crustal. EFc calculations indicated that samples were not enriched with Fe and Cr but were, fairly to extremely, enriched with Zn, Cd, Ni, Pb and Cu. Factor component analysis with varimax-normalized rotation was conducted to find the probable sources of the measured species. This resulted in two factors with eigenvalues greater than unity. Factor 1 showed an anthropogenic source, mostly industrial combustion and local traffic emissions, for Zn, Cd, Ni, Pb, and Cu while factor 2 showed a crustal contribution for Al, Fe and Cr.
在本研究中,对在德黑兰市中心一个地点采集的53个湿大气降水样本(雪和雨水)中的痕量金属锌、镉、铬、镍、铅、铜、铁和铝进行了测量。样本于2011年和2012年11月至5月期间,使用配备高密度聚乙烯漏斗的大容量采样器在市中心一栋建筑物的屋顶上采集。过滤后的样本中的痕量金属用ICP-MS进行测量。结果的统计分析表明,主要源自地壳的元素铝的测量平均浓度最高。pH值范围为4.2至7.1,平均值为5.1。以铝作为参考地壳物质,计算了与地壳物质中元素相对丰度相关的地壳富集因子(EFc)。EFc计算表明,样本中铁和铬未富集,但锌、镉、镍、铅和铜有一定程度至极高程度的富集。进行了具有方差最大化归一化旋转的因子成分分析,以找出被测物种的可能来源。这产生了两个特征值大于1的因子。因子1显示锌、镉、镍、铅和铜的人为来源,主要是工业燃烧和当地交通排放,而因子2显示铝、铁和铬的地壳贡献。