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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Flow dependent water quality impacts of historic coal and oil shale mining in the Almond River catchment, Scotland
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Flow dependent water quality impacts of historic coal and oil shale mining in the Almond River catchment, Scotland

机译:苏格兰杏仁河流域历史煤和油页岩开采的流量相关水质影响

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摘要

The Almond River catchment in Central Scotland has experienced extensive coal mining during the last 300 years and also provides an example of enduring pollution associated with historic unconventional hydrocarbon exploitation from oil shale. Detailed spatial analysis of the catchment has identified over 300 abandoned mine and mine waste sites, comprising a significant potential source of mine related contamination. River water quality data, collected over a 15 year period from 1994 to 2008, indicates that both the coal and oil shale mining areas detrimentally impact surface water quality long after mine abandonment, due to the continued release of Fe and SO_4~(2-) associated with pyrite oxidation at abandoned mine sites. Once in the surface water environment Fe and SO_4~(2-) display significant concentration-flow dependence: Fe increases at high flows due to the re-suspension of river bed Fe precipitates (Fe(OH)_3); SO_4~(2-) concentrations decrease with higher flow as a result of dilution. Further examination of Fe and SO_4 loading at low flows indicates a close correlation of Fe and SO_4~(2-) with mined areas; cumulative low flow load calculations indicate that coal and oil shale mining regions contribute 0.21 and 0.31 g/s of Fe, respectively, to the main Almond tributary. Decreases in Fe loading along some river sections demonstrate the deposition and storage of Fe within the river channel. This river bed Fe is re-suspended with increased flow resulting in significant transport of Fe downstream with load values of up to 50 g/s Fe. Interpretation of major ion chemistry data for 2005-2006 indicates significant increases in Ca~(2+), Mg~(2+) and HCO_3~- in coal mined areas probably as a result of the buffering of proton acidity in mine waters; in the oil shale areas Na~- and Cl~- become increasing dominant possibly associated with increased urbanisation and saline pore water discharge from unprocessed oil shale waste. The study demonstrates the importance of considering the cumulative impact of point and diffuse contamination sourced from numerous small coal and oil shale mine sites on surface water quality.
机译:苏格兰中部的杏仁河流域在过去300年中经历了广泛的煤炭开采,也提供了与历史悠久的油页岩非常规油气开采相关的持久污染的例子。对流域的详细空间分析已确定了300多个废弃的矿山和矿山废料场,其中包括与矿山有关的污染的重要潜在来源。从1994年至2008年的15年中收集的河流水质数据表明,由于Fe和SO_4〜(2-)的持续释放,煤和油页岩矿区都对矿山废弃后很长一段时间的地表水质量产生了不利影响。与废弃矿场的黄铁矿氧化有关。一旦在地表水环境中,Fe和SO_4〜(2-)就表现出明显的浓度-流量依赖性:由于河床的再悬浮,Fe沉淀物(Fe(OH)_3)的重载导致Fe在高流量时增加;稀释导致SO_4〜(2-)浓度随流量增加而降低。进一步检查低流量下的Fe和SO_4负荷表明,Fe和SO_4〜(2-)与采空区密切相关。累积的低流量负荷计算表明,煤和油页岩开采地区分别对主要杏仁支流贡献了0.21和0.31 g / s的铁。沿某些河段的铁负荷减少表明河道内铁的沉积和存储。该河床中的铁被重新悬浮,流量增加,导致铁向下游的大量迁移,负载值高达50 g / s。对2005-2006年主要离子化学数据的解释表明,煤矿区Ca〜(2 +),Mg〜(2+)和HCO_3〜-的显着增加可能是由于矿泉水中质子酸度的缓冲所致。在油页岩地区,Na〜-和Cl〜-占主导地位,这可能与城市化进程加快以及未加工的油页岩废物中的盐分孔隙水排放有关。这项研究表明,考虑从众多小型煤和油页岩矿场获得的点污染和扩散污染对地表水质量的累积影响非常重要。

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