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Sediment-associated contaminant transport and storage dynamics in the Quesnel River from the Mount Polley Mine disaster

机译:波利山矿山灾害在奎斯内尔河中与沉积物有关的污染物迁移和存储动态

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摘要

In August 2014, the tailings storage facility of the Mount Polley copper-gold mine was breached releasing ~25 million m3 of tailings water and solids into Polley Lake and Hazeltine Creek, which scoured local overburden (1.2 million m3), and deposited these materials in Quesnel Lake. This study examined temporal and spatial movements of sediment-associated elements in Quesnel River, downstream of the lake, between August 2014 and August 2015. Suspended river sediment was collected using active and passive samplers (a continuous-flow centrifuge and time-integrated samplers), while discrete bed sediment was collected using a re-suspension technique. Results indicated elevated trace element levels, especially copper, with significant differences between element concentrations at the upstream site, closer to the breach, compared to downstream sites. Contamination indices and comparison to sediment quality guidelines indicated contamination was present in the river and varied seasonally predominantly driven by Quesnel Lake’s autumnal cooling and overturns.
机译:2014年8月,波利山铜金矿的尾矿存储设施遭到破坏,向波利湖和榛树溪释放了约2500万立方米的尾矿水和固体,从而冲刷了当地的覆盖层(120万立方米),并将这些材料沉积在奎斯内尔湖。这项研究调查了2014年8月至2015年8月之间湖下游Quesnel河中沉积物相关元素的时空变化。使用主动和被动采样器(连续流离心机和时间积分采样器)收集悬浮的河底沉积物。 ,同时使用再悬浮技术收集离散的床沉积物。结果表明,痕量元素的水平升高,尤其是铜,与下游位置相比,上游位置(更靠近缺口)的元素浓度之间存在显着差异。污染指数和与沉积物质量准则的比较表明,河流中存在污染,并且季节性变化主要是由于Quesnel湖的秋季降温和倾覆而造成的。

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