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The Applicability of the Distribution Coefficient, KD, Based on Non-Aggregated Particulate Samples from Lakes with Low Suspended Solids Concentrations

机译:分布系数KD的适用性基于低悬浮物浓度湖泊的非聚集颗粒样品

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摘要

Separate phases of metal partitioning behaviour in freshwater lakes that receive varying degrees of atmospheric contamination and have low concentrations of suspended solids were investigated to determine the applicability of the distribution coefficient, KD. Concentrations of Pb, Ni, Co, Cu, Cd, Cr, Hg and Mn were determined using a combination of filtration methods, bulk sample collection and digestion and Inductively Coupled Plasma-Mass Spectrometry (ICP-MS). Phytoplankton biomass, suspended solids concentrations and the organic content of the sediment were also analysed. By distinguishing between the phytoplankton and (inorganic) lake sediment, transient variations in KD were observed. Suspended solids concentrations over the 6-month sampling campaign showed no correlation with the KD (n = 15 for each metal, p > 0.05) for Mn (r2 = 0.0063), Cu (r2 = 0.0002, Cr (r2 = 0.021), Ni (r2 = 0.0023), Cd (r2 = 0.00001), Co (r2 = 0.096), Hg (r2 = 0.116) or Pb (r2 = 0.164). The results implied that colloidal matter had less opportunity to increase the dissolved (filter passing) fraction, which inhibited the spurious lowering of KD. The findings conform to the increasingly documented theory that the use of KD in modelling may mask true information on metal partitioning behaviour. The root mean square error of prediction between the directly measured total metal concentrations and those modelled based on the separate phase fractions were ± 3.40, 0.06, 0.02, 0.03, 0.44, 484.31, 80.97 and 0.1 μg/L for Pb, Cd, Mn, Cu, Hg, Ni, Cr and Co respectively. The magnitude of error suggests that the separate phase models for Mn and Cu can be used in distribution or partitioning models for these metals in lake water.
机译:研究了淡水湖中金属分配行为的不同阶段,该阶段接受了不同程度的大气污染并具有低浓度的悬浮固体,以确定分布系数KD的适用性。使用过滤方法,大量样品收集和消解以及电感耦合等离子体质谱法(ICP-MS)的组合测定Pb,Ni,Co,Cu,Cd,Cr,Hg和Mn的浓度。还分析了浮游植物的生物量,悬浮物浓度和沉积物的有机物含量。通过区分浮游植物和(无机)湖泊沉积物,可以观察到KD的瞬时变化。在六个月的采样过程中,悬浮的固体浓度与锰(r2 = 0.0063),铜(r2 = 0.0002,铬(r2 = 0.021),镍(K = 15对每种金属,p> 0.05)无关。 (r2 = 0.0023),Cd(r2 = 0.00001),Co(r2 = 0.096),Hg(r2 = 0.116)或Pb(r2 = 0.164)。结果表明,胶体物质增加溶解度的机会较小(过滤器通过这一发现与越来越多的文献报道有关,即在建模中使用KD可能掩盖了有关金属分配行为的真实信息时,直接测量的总金属浓度与基于分离相分数建模的铅,镉,锰,铜,汞,镍,铬和钴的误差分别为±3.40、0.06、0.02、0.03、0.44、484.31、80.97和0.1μg/ L。表明锰和铜的独立相模型可以用于这些的分布或分配模型湖水中的金属。

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