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Grain size partitioning of mercury in sediments of the middle Odra river (Germany/Poland)

机译:奥德河中部(德国/波兰)沉积物中汞的粒度分配

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摘要

The aim of this study is to determine the distribution of mercury in different grain size fractions of surface sediments from the middle course of the Odra river. Mercury concentrations were determined in bulk sediments of different grain size fractions using the cold vapor atomic fluorescence spectrometry method. The total mercury concentration in bulk sediments varied from 0.051 to 1.31 mg/kg dry weight. The concentration of total mercury was determined in the grain size fractions < 0.2, 0.2 -0.5,0.5-1.0, 1.0 - 2.0 and > 2.0 mm to be (in mg/kg d. w.): 0.118- 2.99, 0.033 - 0.99, 0.034 -1.17, 0.035 - 1.97 and 0.017 - 3.65, respectively. Gradual decrease in the mercury concentration with increasing grain size from fine to coarse fraction has been observed only for sediments taken from the riverbed. Although, no similar gradual decrease in the mercury concentrations has been observed for sediments from the river-banks, finer sediments (< 0.2 mm) still tend to show higher concentrations of mercury.
机译:这项研究的目的是确定奥德拉河中游不同表面沉积物的不同粒度部分中汞的分布。使用冷蒸气原子荧光光谱法测定了不同粒度分数的块状沉积物中的汞浓度。散装沉积物中的总汞浓度为0.051至1.31 mg / kg干重。确定的总汞浓度在<0.2、0.2 -0.5、0.5-1.0、1.0-2.0和> 2.0 mm的粒度级分中(以mg / kg dw为单位):0.118- 2.99,0.033-0.99,0.034-分别为1.17、0.035-1.97和0.017-3.65。仅从河床取下的沉积物才观察到汞浓度随粒度的增加而从细级到粗级逐渐降低。尽管未观察到来自河岸的沉积物的汞浓度有类似的逐渐下降,但较细的沉积物(<0.2 mm)仍倾向于显示较高的汞浓度。

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