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Determination of organotin compounds in coastal sediment pore-water by diffusive gradients in thin-films (DGT) technique

机译:用薄膜扩散梯度(DGT)技术测定沿海沉积物孔隙水中有机锡化合物

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摘要

Organotin compounds still present a high risk to biota in the aquatic environment. Measuring the behaviour of the freely dissolved fractions of these compounds in sediment compartments is challenging, with costly and sensitive analytical techniques required for their measurement. Diffusive gradients in thin-films (DGT) allow for the uptake and pre-concentration of analytes in a binding gel and is used to measure dissolved metals and some organic compounds. The utility of novel silica-bound sorbents (C8, C18, mixed phases) as DGT binding gels for the sequestration of organotins in the marine environment was the primary focus of work in this project. The C8 sorbent showed the optimum performance in the uptake and recovery of organotins across pH, ionic strength and in filtered sea water. It was used subsequently as the binding layer in DGT sediment devices (160 mm × 34 mm) overlaid with a mixed-cellulose ester membrane (0.45 μm) as the single diffusion layer. These were used to investigate pore water mobilisation and concentrations of organotins in coastal sediment cores collected from a contaminated site. Organotins demonstrated a non-sustained uptake scenario, with DGT flux and freely dissolved concentrations in pore water measured to decline at 1 cm depth intervals over deployments of 2-28 days. Using time series, concentrations in pore water at t = 0 were calculated providing empirical pore water depletion curves for sediment cores. Using standard laboratory instrumentation (i.e. gas chromatography-mass spectrometry) low limits of detection were achieved (TBT = 0.4 ng L after 2 weeks of sampling).
机译:有机锡化合物仍然对水生环境中的生物群构成高风险。测量这些化合物在沉淀室内的自由溶解部分的行为具有挑战性,因为它们的测量需要昂贵且敏感的分析技术。薄膜中的扩散梯度(DGT)允许结合凝胶中分析物的吸收和预富集,并用于测量溶解的金属和某些有机化合物。新型二氧化硅结合的吸附剂(C8,C18,混合相)作为DGT结合凝胶用于海洋环境中有机锡螯合的实用性是该项目的主要工作重点。 C8吸附剂在pH,离子强度和过滤海水中的有机锡的吸收和回收方面显示出最佳性能。随后将其用作DGT沉积装置(160 mm×34 mm)中的粘合层,该层上铺有混合纤维素酯膜(0.45μm)作为单扩散层。这些用于调查孔隙水的动员和从受污染地点收集的沿海沉积物芯中有机锡的浓度。有机锡显示出非持续摄取的情况,在部署2-28天后,DGT通量和孔隙水中自由溶解的浓度在1厘米深度处下降。使用时间序列,计算出t = 0时孔隙水的浓度,提供了沉积物岩心的经验性孔隙水消耗曲线。使用标准的实验室仪器(即气相色谱-质谱)可实现低检测限(采样2周后,TBT = 0.4 ng L)。

著录项

  • 作者

    Cole Russell Francis;

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  • 年度 2016
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  • 原文格式 PDF
  • 正文语种 eng
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