School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth PL4 8AA, UK.
Water Res. 2010 Jul;44(14):4204-16. doi: 10.1016/j.watres.2010.05.022. Epub 2010 May 24.
Silver is one of the most toxic elements for the marine microbial and invertebrate community. However, little is known about the distribution and behaviour of dissolved silver in marine systems. This paper reports data on dissolved and sediment-associated silver in European estuaries and coastal waters which have been impacted to different extents by past and present anthropogenic inputs. This is the first extended dataset for dissolved silver in European marine waters. Lowest dissolved silver concentrations were observed in the Gullmar Fjord, Sweden (8.9 +/- 2.9 pM; x +/- 1sigma), the Tamar Estuary, UK (9.7 +/- 6.2 pM), the Fal Estuary, UK (20.6 +/- 8.3 pM), and the Adriatic Sea (21.2 +/- 6.8 pM). Enhanced silver concentrations were observed in Atlantic coastal waters receiving untreated sewage effluent from the city of A Corũna, Spain (243 +/- 195 pM), and in the mine-impacted Restronguet Creek, UK (91 +/- 71 pM). Anthropogenic wastewater inputs were a source of dissolved silver in the regions studied, with the exception of the Gullmar Fjord. Remobilisation of dissolved silver from historically contaminated sediments, resulting from acid mine drainage or sewage inputs, provided an additional source of dissolved silver to the estuaries. The ranges in the log particle-water partition coefficient (K(d)) values of 5-6 were similar for the Tamar and Mero estuaries and agreed with reported values for other estuaries. These high K(d) values indicate the particle reactive nature of silver with oxic sediments. In contrast, low K(d) values (1.4-2.7) were observed in the Fal system, which may have been due to enhanced benthic inputs of dissolved silver coupled to limited scavenging of silver on to sediments rich in Fe oxide.
银是海洋微生物和无脊椎动物群落中最具毒性的元素之一。然而,对于海洋系统中溶解态银的分布和行为知之甚少。本文报告了欧洲河口和沿海水域中溶解态和沉积物结合态银的数据,这些水域过去和现在都受到人为输入的不同程度的影响。这是欧洲海洋水中溶解态银的第一个扩展数据集。在瑞典的古尔马峡湾(Gullmar Fjord)、英国的塔玛尔河口(Tamar Estuary)、英国的法尔河口(Fal Estuary)和亚得里亚海(Adriatic Sea),观察到的溶解银浓度最低(分别为 8.9 +/- 2.9 pM、9.7 +/- 6.2 pM、20.6 +/- 8.3 pM 和 21.2 +/- 6.8 pM)。在西班牙的阿科鲁尼亚市接受未经处理的污水排放的大西洋沿海水域以及受矿区影响的英国雷斯托格涅克溪(Restronguet Creek),观察到增强的银浓度(分别为 243 +/- 195 pM 和 91 +/- 71 pM)。除了古尔马峡湾外,研究区域的人为废水输入是溶解银的来源。由于酸性矿山排水或污水输入,从历史上受污染的沉积物中重新释放出溶解态银,为河口提供了额外的溶解态银源。塔马尔和梅罗河口的对数颗粒-水分配系数(K(d))值范围为 5-6,与其他河口的报道值一致。这些高 K(d)值表明银与含氧沉积物具有颗粒反应性。相比之下,在法尔系统中观察到低 K(d)值(1.4-2.7),这可能是由于溶解态银的底栖输入增加,同时铁氧化物丰富的沉积物对银的吸附有限。