Bird Graham
School of Environment, Natural Resources and Geography, Bangor University, Bangor, Gwynedd, LL57 2UW, UK.
Environ Sci Pollut Res Int. 2016 Dec;23(23):23456-23466. doi: 10.1007/s11356-016-7400-z. Epub 2016 Sep 10.
Globally, thousands of kilometres of rivers are degraded due to the presence of elevated concentrations of potentially harmful elements (PHEs) sourced from historical metal mining activity. In many countries, the presence of contaminated water and river sediment creates a legal requirement to address such problems. Remediation of mining-associated point sources has often been focused upon improving river water quality; however, this study evaluates the contaminant legacy present within river sediments and attempts to assess the influence of the scale of mining activity and post-mining remediation upon the magnitude of PHE contamination found within contemporary river sediments. Data collected from four exemplar catchments indicates a strong relationship between the scale of historical mining, as measured by ore output, and maximum PHE enrichment factors, calculated versus environmental quality guidelines. The use of channel slope as a proxy measure for the degree of channel-floodplain coupling indicates that enrichment factors for PHEs in contemporary river sediments may also be the highest where channel-floodplain coupling is the greatest. Calculation of a metric score for mine remediation activity indicates no clear influence of the scale of remediation activity and PHE enrichment factors for river sediments. It is suggested that whilst exemplars of significant successes at improving post-remediation river water quality can be identified; river sediment quality is a much more long-lasting environmental problem. In addition, it is suggested that improvements to river sediment quality do not occur quickly or easily as a result of remediation actions focused a specific mining point sources. Data indicate that PHEs continue to be episodically dispersed through river catchments hundreds of years after the cessation of mining activity, especially during flood flows. The high PHE loads of flood sediments in mining-affected river catchments and the predicted changes to flood frequency, especially, in many river catchments, provides further evidence of the need to enact effective mine remediation strategies and to fully consider the role of river sediments in prolonging the environmental legacy of historical mine sites.
在全球范围内,由于历史金属采矿活动产生的潜在有害元素(PHEs)浓度升高,数千公里的河流受到了污染。在许多国家,受污染的河水和河流沉积物的存在使得解决这些问题成为一项法律要求。与采矿相关的点源修复通常侧重于改善河流水质;然而,本研究评估了河流沉积物中存在的污染物遗留问题,并试图评估采矿活动规模和采矿后修复对当代河流沉积物中PHE污染程度的影响。从四个典型流域收集的数据表明,以矿石产量衡量的历史采矿规模与根据环境质量准则计算的最大PHE富集系数之间存在密切关系。使用河道坡度作为河道与河漫滩耦合程度的替代指标表明,在河道与河漫滩耦合程度最大的地方,当代河流沉积物中PHE的富集系数可能也是最高的。对矿山修复活动的指标得分计算表明,修复活动规模对河流沉积物的PHE富集系数没有明显影响。研究表明,虽然可以确定在改善修复后河流水质方面取得显著成功的范例;但河流沉积物质量是一个更持久的环境问题。此外,研究还表明,针对特定采矿点源的修复行动并不会迅速或轻易地改善河流沉积物质量。数据表明,在采矿活动停止数百年后,PHEs仍会通过河流集水区间歇性地扩散,尤其是在洪水期间。受采矿影响的河流集水区洪水沉积物中的高PHE负荷以及洪水频率的预测变化,特别是在许多河流集水区,进一步证明了制定有效的矿山修复策略以及充分考虑河流沉积物在延长历史矿山环境遗留问题方面作用的必要性。