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首页> 外文期刊>Analytica chimica acta >Monitoring acid-volatile sulphide by a fast scan voltammetric method:application to mercury contamination studies in salt marsh sediments
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Monitoring acid-volatile sulphide by a fast scan voltammetric method:application to mercury contamination studies in salt marsh sediments

机译:通过快速扫描伏安法监测酸挥发性硫化物:在盐沼沉积物中汞污染研究中的应用

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The present work demonstrates the application of fast scan linear sweep cathodic stripping voltammetry to the determination of acid-volatile sulphide (AVS) in salt marsh sediments.This approach combines very fast analysis with relatively high sensitivity without the need for additional reagents or derivatization procedures.The purge-and-trap AVS methodology was used.The sulphide content in the trapping NaOH solution was directly measured by voltammetry with a high scan rate (1000 mV s~(-1)).The limit of detection (3sigma) was 0.34 (mumol L~(-1) for a deposition time of 5 s.Vertical distribution of AVS in sediments was determined in salt marsh sediments of a Portuguese coastal lagoon vegetated with H.portulacoides and correlated to the total dissolved mercury content in pore waters.At the depth of higher root biomass (around 20 cm),AVS concentrations (range 0.24-24.8 mumolg~(-1)) were low in comparison to other depths,probably due to modifications in sediments that occur in the vicinity of the roots.The highest dissolved mercury concentrations (835 and 675 ngL~(-1)),were found at the surface layer and at 20cm depth,with an opposite trend from that of AVS.A possible explanation is that root activity reduced AVS concentrations at the depth of higher root biomass and resulted in elevated pore water concentrations of mercury.Concentrations of mercury in pore water from layers above and below the high root biomass were consistently lower (less than 152ngL~(-1)).
机译:本工作证明了快速扫描线性扫描阴极溶出伏安法在测定盐沼沉积物中酸挥发性硫化物(AVS)中的应用,该方法结合了非常快速的分析和相对较高的灵敏度,而无需其他试剂或衍生化程序。采用吹扫捕集AVS方法,通过伏安法以高扫描速率(1000 mV s〜(-1))直接测量捕获的NaOH溶液中的硫化物含量,检出限(3sigma)为0.34( mmol L〜(-1)沉积时间为5 s。在葡萄牙滨海泻湖中,H.portulacoides植被的盐沼沉积物中确定了AVS在沉积物中的垂直分布,并与孔隙水中的总溶解汞含量相关。较高的根生物量深度(约20 cm),AVS浓度(0.24-24.8 mumolg〜(-1))与其他深度相比较低,这可能是由于附近沉积物发生了变化在表层和20cm深度处发现最高的溶解汞浓度(835和675 ngL〜(-1)),与AVS趋势相反。可能的解释是根系活性降低了AVS高根生物量深度处的汞浓度较高,导致孔隙水中的汞浓度升高。高根生物质上方和下方各层孔隙水中的汞浓度始终较低(小于152ngL〜(-1))。

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