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微潮三角洲系统中汞形态的行为:伊松佐河口(亚得里亚海北部)。

Behaviour of Hg species in a microtidal deltaic system: the Isonzo River mouth (northern Adriatic Sea).

作者信息

Covelli Stefano, Piani Raffaella, Kotnik Joze, Horvat Milena, Faganeli Jadran, Brambati Antonio

机构信息

Department of Geological, Environmental and Marine Sciences, University of Trieste, Via E.Weiss 2, 34127 Trieste, Italy.

出版信息

Sci Total Environ. 2006 Sep 1;368(1):210-23. doi: 10.1016/j.scitotenv.2005.09.089. Epub 2005 Nov 11.

Abstract

Mercury species in the highly stratified water column of the Isonzo River mouth (northern Adriatic Sea) were investigated in February, May and August 2002 (low-normal fluvial discharge). Total, dissolved and particulate mercury (Hg) and methylmercury (MeHg) were measured and their concentrations were related to physico-chemical parameters in terms of temperature, salinity, turbidity, O(2) concentrations and total suspended matter (TSM) as well as particulate organic carbon (POC) content. Particulate Hg and MeHg are well correlated to medium-fine silty suspended sediment and organic matter, respectively. Desorption of Hg from particles in the brackish layer was observed. Due to the presence of a saltwedge, the lower river course seems to be a trap for Hg carried by fluvial waters. MeHg normally decreases approaching the sea but the local increase in the inner zone of the saltwedge could be related to methylation processes in the bottom water layer. Hg export is effective only during medium and high riverine flows acting as an important source of Hg into the northern Adriatic and the adjacent lagoon system.

摘要

2002年2月、5月和8月(河流低至正常流量)对伊松佐河口(亚得里亚海北部)高度分层水柱中的汞形态进行了调查。测定了总汞、溶解汞、颗粒汞(Hg)和甲基汞(MeHg),并根据温度、盐度、浊度、O₂浓度、总悬浮物(TSM)以及颗粒有机碳(POC)含量等理化参数对其浓度进行了关联分析。颗粒汞和甲基汞分别与中细粉质悬浮沉积物和有机物密切相关。观察到咸淡水层中汞从颗粒上的解吸现象。由于存在盐楔,下游河道似乎是河水携带汞的一个汇集区。甲基汞通常在靠近海洋的地方减少,但盐楔内部区域的局部增加可能与底层水层中的甲基化过程有关。汞的输出仅在中等和高河流流量期间有效,河流是亚得里亚海北部和相邻泻湖系统汞的重要来源。

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