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首页> 外文期刊>Journal of Contaminant Hydrology >Attenuation of landfill leachate by UK Triassic sandstone aquifer materials 1. Fate of inorganic pollutants in laboratory columns
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Attenuation of landfill leachate by UK Triassic sandstone aquifer materials 1. Fate of inorganic pollutants in laboratory columns

机译:英国三叠纪砂岩含水层材料对垃圾渗滤液的衰减作用1.实验室色谱柱中无机污染物的去向

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摘要

The attenuation of inorganic contaminants in acetogenic and methanogenic landfill leachate by calcareous and carbonate-deficient, oxide--rich Triassic sandstone aquifer materials from the English Midlands was examined in laboratory columns. Aqueous equilibrium speciation mod- elling, simple transport modelling and chemical mass balance approaches are used to evaluate the key processes and aquifer geochemical properties controlling contaminant fate. The results indicate that leachate-rock interactions are dominated by ion--exchange processes, acid-base and redox reactions and sorption/precipitation of metal species. Leachate NH_4 is attenuated by cation exchange with the aquifer sediments; however, NH# migration could be described with a simple model using retardation factors. Organic acids in the acetogenic leachate buffered the system pH at low levels during flushing of the calcareous aquifer material. In contrast, equilibrium with Al oxyhydroxide phases initially buffered pH (~ 4.5) during flushing of the carbonate-deficient sandstone with methanogenic leachate.
机译:在实验室色谱柱中检测了来自英国中部地区的钙质和碳酸盐含量低,富含氧化物的三叠纪砂岩含水层材料对产乙酸和产甲烷的垃圾渗滤液中无机污染物的衰减。水平衡物种形成模型,简单的运输模型和化学物质平衡方法用于评估关键过程和控制污染物命运的含水层地球化学性质。结果表明,渗滤液与岩石的相互作用主要受离子交换过程,酸碱和氧化还原反应以及金属物质的吸附/沉淀作用的影响。通过与含水层沉积物的阳离子交换,渗滤液NH_4减弱。但是,可以使用延迟因子通过简单模型描述NH#迁移。产乙酸的渗滤液中的有机酸在石灰质含水层材料冲洗期间将系统pH缓冲在较低水平。相比之下,氢氧化铝铝相的平衡最初在用产甲烷浸出液冲洗碳酸盐缺乏的砂岩时缓冲了pH(〜4.5)。

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