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首页> 外文期刊>Journal of Contaminant Hydrology >Integration of field measurements and reactive transport modelling to evaluate contaminant transport at a sulfide mine tailings impoundment
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Integration of field measurements and reactive transport modelling to evaluate contaminant transport at a sulfide mine tailings impoundment

机译:现场测量和反应性运输模型的集成,以评估硫化矿尾矿库中污染物的运输

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摘要

Over a decade of field observations including geochemical, mineralogical and hydrological information are available on the generation of acid mine drainage from the Pistol Dam region of the P-area of Inco's tailings impoundment in Copper Cliff, Ontario. This work focuses on the integration and quantitative assessment of this data set using reactive transport modeling. The results of the reactive transport simulations are in general agreement with the field observations; however, exact agreement between the field and simulated results was not the objective of this study, and was not attained. Many factors contribute to the discrepancies between the field observations and simulation results including geochemical and hydrogeological complexities and necessary model simplifications. For example, fluctuating water levels observed at the site were averaged and described using a steady state flow system. In addition, the lack of representative thermodynamic and rate expression data contributed to the discrepancies between observations and simulation results, thus further research into the applicability of laboratory-derived thermodynamic and rate expression data to field conditions could minimize these discrepancies. Despite the discrepancies between the field observations and simulated results, integrating field observations with numerical modelling of the P-area tailings impoundment allowed for a more complete understanding of what affects the complex geochemical reactions.
机译:十多年来的现场观察包括地球化学,矿物学和水文信息,可用于从安大略省铜崖的Inco尾矿库P区的Pistol坝区产生的酸性矿山排水。这项工作着重于使用反应性运输模型对该数据集进行整合和定量评估。反应性输运模拟的结果与现场观测结果基本吻合。但是,该领域与模拟结果之间的确切一致性不是本研究的目的,并且没有实现。许多因素导致了野外观测和模拟结果之间的差异,包括地球化学和水文地质方面的复杂性以及必要的模型简化。例如,使用稳态流量系统对现场观测到的波动水位进行平均并进行描述。此外,缺乏代表性的热力学和速率表达数据导致了观测值与模拟结果之间的差异,因此,进一步研究实验室衍生的热力学和速率表达数据在现场条件下的适用性可以最大程度地减少这些差异。尽管现场观测结果和模拟结果之间存在差异,但将现场观测结果与P区域尾矿蓄水量的数值模型集成在一起,可以更全面地了解影响复杂地球化学反应的因素。

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