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A Siderite-Amended Reactive Cap for High-pH Sediments of Onondaga Lake, New York

机译:用于纽约奥尼达加湖高pH沉积物的菱铁矿修饰反应帽

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Background/Objectives. Contaminated sediments in some areas of Onondaga Lake arecharacterized by elevated porewater pH (greater than 10 and up to 12.5). The finalremedial design includes capping of approximately 170 acres of the lake bed for habitatrestoration. Siderite, a naturally occurring iron ore, was identified as the most suitable capamendment for long-term pH control and buffering. A series of laboratory and modelinginvestigations were undertaken to determine site-specific performance and effectiveness,develop spatially optimized siderite doses to meet multiple performance criteria, andassess sensitivity of cap performance to, and develop methods for evaluating, deviationsfrom the design specifications during construction. Construction of the siderite-amendedcap was initiated in 2012.Approach/Activities. Batch tests were conducted to investigate porewater pH bufferingand neutralization rates by siderite. Preliminary cap modeling using PHREEQC, withreaction rates calibrated to batch test data, indicated a relatively low siderite dose(~1 lbs/ft~2 of cap surface) would meet cap performance requirements. The low sideritedemand also pointed to a potential concern that pore-scale bypassing could impact bulkreactivity at field-scale and that the cap model may have overpredicted effectiveness.Column studies were subsequently carried out to assess whether pore-scale flow couldimpact macroscopic pH neutralization rates under cap conditions. Reactive transportmodeling was also performed to develop optimal siderite doses on an area-specific basis,considering spatial distributions of porewater pH, upwelling velocities and expectedconsolidation following cap construction. Sensitivity analyses were also conducted toevaluate the sensitivity of cap performance to uneven vertical distribution of amendmentwithin the chemical isolation (CI) layer due to segregation during emplacement. Fieldmethods qualitatively verifying the presence of siderite within the sand cap matrix duringconstruction were also developed.Results/Lessons Learned. Column tests confirmed that pore-scale effects had anegligible impact on bulk reactivity for siderite doses as low as 1 lbs/ft2 distributed withina 0.5 ft thick CI layer. Transient simulations show that cap consolidation flux stronglyinfluences initial porewater pH neutralization, and indicate that pH above the CI layercould remain elevated for up to several years after cap construction, as the initiallyrapidly expressed high pH porewater is flushed by neutralized porewater. Long-termperformance is tied to porewater pH and average groundwater upwelling velocities.Optimized area-specific doses taking these factors into account ranged from 1.0 to 3.5
机译:背景/目标。奥农达加湖某些地区的受污染沉积物是 其特征是孔隙水的pH值升高(大于10且高达12.5)。决赛 补救性设计包括将约170英亩的湖床封盖用于栖息地 恢复。菱铁矿(一种天然存在的铁矿石)被确定为最合适的矿顶 长期pH控制和缓冲的修正。一系列的实验室和建模 进行了调查以确定特定地点的性能和有效性, 开发空间优化的菱铁矿剂量,以满足多种性能标准,并且 评估瓶盖性能对偏差的敏感性,并开发评估偏差的方法 根据施工期间的设计规格。修整的菱铁矿的构造 上限于2012年启动。 方法/活动。进行批次测试以研究孔隙水的pH缓冲 菱铁矿的中和率。使用PHREEQC进行的初步瓶盖建模 校准至批处理数据的反应速率,表明相对较低的菱铁矿剂量 (约1 lbs / ft〜2的瓶盖表面)将满足瓶盖性能要求。低菱铁矿 需求还指出了潜在的担忧,即孔垢旁路可能会影响体积 现场规模的反应性和上限模型可能具有过高预测的有效性。 随后进行了柱研究,以评估孔垢流是否可以 影响上限条件下的宏观pH中和率。反应性运输 还进行了建模以在特定区域内开发最佳菱铁矿剂量, 考虑孔隙水pH值的空间分布,上升速度和预期 封顶施工后进行合并。还进行了敏感性分析,以 评估瓶盖性能对修正物不均匀垂直分布的敏感性 由于放置过程中的隔离,导致化学隔离(CI)层中的碳纳米管泄漏。场地 定性验证砂帽基质中菱铁矿存在的方法。 建设也得到了发展。 结果/经验教训。柱测试证实,孔垢效应具有 菱铁矿剂量低至1 lbs / ft2分布时对整体反应性的影响可忽略不计 0.5英尺厚的CI层。瞬态仿真表明,瓶盖固结力很强 影响初始孔隙水的pH中和,并表明pH高于CI层 瓶盖建造后,可能会保持高架状态长达数年之久,因为最初 快速表达的高pH孔隙水被中和的孔隙水冲刷。长期 性能与孔隙水的pH值和地下水的平均上升速度有关。 考虑到这些因素的最佳区域特定剂量范围为1.0到3.5

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