Harmful Metal Export from Abandoned Mines Controlled by Hydrodynamic and Biogeochemical Drivers

IF 4.3 Q1 ENVIRONMENTAL SCIENCES
Anita Alexandra Sanchez*, Conrad Jackisch, Michel Oelschlägel, Sabrina Hedrich and Maximilian P. Lau, 
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引用次数: 0

Abstract

Abandoned mines are significant contaminant sources to rivers and lakes, with metal(loid) leaching and acid drainage impacting water quality and ecosystem function. While mine drainage is conventionally assumed to contribute contaminants continuously over decadal time scales, recent findings indicate episodic pulses of metal(loid) export with uncertain drivers. Here, we investigate a former lead–silver-zinc mine (Reiche Zeche, Germany) that drains directly into Elbe River tributaries, identifying spatial and temporal peaks in contaminant release, i.e., “hotspots” of reactivity. Through biogeochemical monitoring and molecular profiling of dissolved organic matter (DOM) and microbial communities, we reveal dynamic contaminant sources. One hotspot exhibited a release pattern controlled by density stratification, in which deeper, isolated layers with iron-oxidizing bacteria intensively accumulated metals and DOM. We demonstrate that specific molecular formulas within DOM are tightly coupled to metals, such that DOM can act as a persistent tracer of hotspot activity while also potentially enhancing metal(loid) complexation, stabilization, and release processes. A broader survey of abandoned mines (n = 28) revealed similar DOM signatures downstream of leaching sites, suggesting similarities in the contaminant release dynamics. These findings provide a framework for novel contaminant monitoring approaches and highlight the need for improved water management strategies at subsurface–surface interfaces in postmining landscapes.

This work provides a unique insight into the hydrological dynamic, biogeochemical functioning, and regional prevalence of contaminant release from (abandoned) subsurface mines.

水动力与生物地球化学驱动控制下废弃矿山有害金属出口
废弃矿山是河流和湖泊的重要污染源,金属(样)浸出和酸性排放影响着水质和生态系统功能。虽然矿山排水通常被认为在十年时间尺度上持续贡献污染物,但最近的研究结果表明,金属(loid)出口的周期性脉冲具有不确定的驱动因素。在这里,我们调查了一个直接排入易北河支流的前铅银锌矿(德国Reiche Zeche),确定了污染物释放的时空峰值,即反应性的“热点”。通过生物地球化学监测和溶解有机物(DOM)和微生物群落的分子谱分析,我们揭示了动态污染源。其中一个热点表现出由密度分层控制的释放模式,在较深的孤立层中,铁氧化细菌密集地积聚金属和DOM。我们证明了DOM中的特定分子式与金属紧密耦合,因此DOM可以作为热点活动的持久示踪剂,同时还可能增强金属(样蛋白)的络合、稳定和释放过程。对废弃矿山(n = 28)的更广泛调查显示,在浸出点下游有类似的DOM特征,这表明污染物释放动力学具有相似性。这些发现为新的污染物监测方法提供了框架,并强调了在采矿后景观中改善地下-地表界面水管理策略的必要性。这项工作为水文动态、生物地球化学功能和(废弃)地下矿山污染物释放的区域流行提供了独特的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
5.40
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0.00%
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