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Pyritization of trace metals in estuarine sediments and the controlling factors: a case in Jiaojiang Estuary of Zhejiang Province, China

机译:河口沉积物中微量金属的黄铁化及其控制因素-以浙江省椒江口为例

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Three undisturbed sediment samples were collected from the intertidal zone of the Jiaojiang Estuary of Zhejiang Province, China. The sediments were found to contain remarkably low concentrations of organic carbon (<0.6%) and acid volatile sulfide (AVS) (<30 μmol g−1). The availability of these two substrates likely constrained sulfate reduction and pyritization of several trace metals, respectively. This was especially true at one station where AVS concentrations in the upper 20 cm averaged less than 0.05 μmol g−1. Although the depth dependence of the degree of trace metal pyritization was generally consistent with expectations based on redox conditions, depth profiles of reactive-metal and pyrite-metal concentrations in several cases revealed more complex behavior and a positive correlation between reactive-metal concentrations and pore water metal concentrations.
机译:从浙江省椒江河口潮间带采集了三个原状沉积物样品。发现沉积物中的有机碳(<0.6%)和酸挥发性硫化物(AVS)的浓度非常低(<30μmolg -1 )。这两种底物的可用性可能分别限制了几种痕量金属的硫酸盐还原和黄铁矿化。在一个站的情况尤其如此,该站的上部20 cm处的AVS浓度平均低于0.05μmolg -1 。尽管痕量金属黄铁化程度的深度依赖性通常与基于氧化还原条件的预期一致,但在某些情况下,活性金属和黄铁矿金属浓度的深度分布显示出更复杂的行为,并且活性金属浓度与孔隙之间呈正相关水金属浓度。

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