斐济Kadavu通道沉积物中微量元素的浓度

S. Garimella, R. Lal, R. Deo, R. Morrison
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引用次数: 2

摘要

研究人员利用中子活化和高分辨率伽马射线能谱技术,从斐济苏瓦半岛和卡达武岛之间的太平洋海底11个地点收集了Grab沉积物,研究了20种元素的浓度。这些沉积物是在距离大陆5-35公里和海洋深度500 - 2000米的地方收集的。将这些沉积物的元素丰度与苏瓦泻湖和其他附近地区的元素丰度进行比较表明,海洋沉积物很可能来自从大陆冲到海洋的沉积物。沉积物也没有显示苏瓦市区工业活动造成任何金属污染的证据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trace element concentrations in sediments from Kadavu passage, Fiji
Grab sediments, collected from 11 locations from the Pacific Ocean floor in the region between Suva Peninsula and Kadavu Island, Fiji, were investigated for concentrations of 20 elements using neutron activation and high-resolution gamma ray spectroscopy techniques. The sediments were collected at distances between 5-35 km from the mainland and at ocean depths ranging from 500 to 2000 m. A comparison of the elemental abundances of these sediments with those of the Suva lagoon and other nearby locations indicates that the ocean sediments are likely to be derived from sediments washed out to sea from the mainland. The sediments also show no evidence of any metal contamination from the industrial activity in the Suva metropolitan area.
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