首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Fractionation, distribution and transport of mercury in rivers and tributaries around Wanshan Hg mining district, Guizhou Province, Southwestern China: Part 2-Methylmercury
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Fractionation, distribution and transport of mercury in rivers and tributaries around Wanshan Hg mining district, Guizhou Province, Southwestern China: Part 2-Methylmercury

机译:中国西南地区贵州省万山汞矿区周围河流和支流中汞的分馏,分布和运输:第2部分-甲基汞

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摘要

Water samples were collected during normal flow (2007) and during a drought period (2008) from five rivers and tributaries draining the Wanshan Hg mining district, Guizhou, China. Unfiltered methylmercury (MeHg) as well as particulate and dissolved fractions of MeHg (P-MeHg, D-MeHg) were measured to assess the spatial and temporal variation of MeHg contamination in the local river system. Most locations (about 80%) displayed higher MeHg concentrations during drought period than during normal discharge conditions. Concentrations of MeHg during the drought period ranged from <0.035 to 11 ng L-1 (geometric mean: 0.43), while during normal flow the concentrations ranged from <0.035 to only 3.4 ng L-1 (geometric mean: 0.21). Concentrations of MeHg were positively correlated with total Hg (THg) concentrations (R-2 = 0.20-0.58, P < 0.001) and inversely related to distance from the calcines, during both sampling periods (R-2 = 0.34 and 0.23, P < 0.001, for low and normal flow, respectively) indicating that calcines may be important sources of MeHg to the downstream environment. Approximately 39% of MeHg was bound to particulates and the rest was transported in the dissolved phase along stretches of the entire river, which was different from THg, as this was mainly transported bound to particulates (commonly more than 80%).
机译:在正常流量(2007年)和干旱时期(2008年)期间,从贵州万山汞矿开采区的五条河流和支流中采集了水样。测量未过滤的甲基汞(MeHg)以及MeHg的颗粒和溶解级分(P-MeHg,D-MeHg),以评估当地河流系统中MeHg污染的时空变化。大多数地区(约80%)在干旱期间显示的MeHg浓度高于正常排放条件。干旱期间MeHg的浓度范围从<0.035至11 ng L-1(几何平均值:0.43),而在正常流量期间,浓度范围从<0.035至仅3.4 ng L-1(几何平均值:0.21)。在两个采样期间内,MeHg的浓度与总Hg(THg)浓度呈正相关(R-2 = 0.20-0.58,P <0.001),与距煅烧炉的距离呈负相关(R-2 = 0.34和0.23,P < 0.001,分别表示低流量和正常流量),这表明煅烧可能是下游环境中MeHg的重要来源。大约39%的MeHg结合到颗粒上,其余的则以溶解相形式沿整个河流延伸,这与THg不同,因为主要是结合颗粒物(通常超过80%)运输。

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