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检测亚得里亚海西部(地中海)沉积物中金属的长期时间趋势。

Detecting long-term temporal trends in sediment-bound metals in the western Adriatic (Mediterranean Sea).

机构信息

Departamento de Química-Física, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz, UNESCO/UNITWIN WiCoP, Campus de Excelencia International del Mar (CEIMAR), Polígono Río San Pedro s/n, Puerto Real 11510, Cádiz, Spain; Centro Interdipartimentale di Ricerca per le Scienze Ambientali (C.I.R.S.A.), University of Bologna, Ravenna Campus, 48123 Ravenna, Italy.

National Research Council-Institute of Marine Sciences (CNR-ISMAR), 40129 Bologna, Italy.

出版信息

Mar Pollut Bull. 2017 Nov 15;124(1):270-285. doi: 10.1016/j.marpolbul.2017.07.026. Epub 2017 Aug 9.

Abstract

Major and trace metal concentrations were determined in western Adriatic sediment cores. Based on sediment chronology, the earliest anthropogenic influence appeared as a Zn and Pb increase in the Po River prodelta starting from ~1914. The increasing contamination signal of these trace metals propagated southward as far as 450km with a growing delay, taking ~10years to reach the south Adriatic Sea. Although greater inventories of excess trace metals in the northern sector pointed to the influence of the intense human activities in the Po River drainage basin and Venice lagoon system, we observed a reduction of excess trace metals from mid-1980s, related to the implementation of stricter environmental regulations on chemical wastewaters. In contrast, an increase in trace metal accumulation in surficial sediment from the 2000s in front of the cities of Ancona and Bari suggested a recent local input of trace metals, probably due to harbor activities.

摘要

对亚得里亚海西部的沉积物岩芯进行了主要和微量元素浓度的测定。根据沉积年代学,最早的人为影响表现为从大约 1914 年开始,波河三角洲的 Zn 和 Pb 增加。这些微量元素的污染信号向南传播,传播距离最远可达 450km,但存在时间延迟,大约需要 10 年才能到达亚得里亚海南部海域。尽管北部地区存在更多的过量微量元素,表明波河流域和威尼斯泻湖系统的人类活动非常强烈,但我们观察到自 20 世纪 80 年代中期以来,过量微量元素的数量有所减少,这与对化学废水实施更严格的环境法规有关。相比之下,安科纳和巴里市前的表层沉积物中微量元素的积累增加表明,最近有局部输入了微量元素,可能是由于港口活动所致。

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