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A three-dimensional mass transport model of the Mannheim Aquifer Storage and Recovery system, Kitchener, Ontario.

机译:曼海姆含水层存储和回收系统的三维大规模运输模型,安大略省基奇纳。

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Simulations of the Mannheim Aquifer Storage and Recovery (ASR) system in Kitchener, Ontario, were completed using a three-dimensional flow and advective-dispersive mass transport model. For all simulations a tracer-based approach was used to follow the movement of injected water throughout the storage and extraction cycles. Research focused on describing the system's response to a yearly cycle comprised of 60 days of injection into the heterogeneous and semi-confined aquifer. This was followed by 180 days of storage, 30 days of recovery, and finally 95 days free of any activity. Prior to simulation of tracer movement, the model was calibrated to pre-injection (steady-state) heads to set the regional gradient which varied between 0.002 and 0.0035. Results showed that migration of injected water had a significant impact on water which replenished the local aquifer or was extracted at off-site wells. Analyses also revealed that only a small proportion of injected water may be extracted at the ASR facility, depending on the layout of recovery wells. Quantitative confirmation of model results is still required to propose a more efficient recovery well configuration.
机译:使用三维流动和对流-弥散物质传输模型,完成了安大略省基奇纳市的曼海姆含水层存储和回收(ASR)系统的模拟。对于所有模拟,都使用基于示踪剂的方法来跟踪注入水在整个存储和提取周期中的运动。研究重点是描述系统对年周期的响应,该周期包括向异质半封闭含水层中注入60天。随后是180天的存储,30天的恢复,最后是95天没有任何活动。在模拟示踪剂运动之前,将模型校准到预注射(稳态)压头,以设置在0.002至0.0035之间变化的区域梯度。结果表明,注入水的迁移对补充局部含水层或从异地井抽出的水有显着影响。分析还显示,取决于回收井的布置,在ASR设施中只能提取一小部分注入的水。仍需要对模型结果进行定量确认,以提出更有效的采油井配置。

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