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In Situ Chemical Oxidation of RDX-Contaminated Groundwater with Permanganate at the Nebraska Ordnance Plant

机译:内布拉斯加州兵工厂用高锰酸盐对RDX污染的地下水进行原位化学氧化

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摘要

Groundwater beneath the former Nebraska Ordnance Plant (NOP) is contaminated with the explosive hexahydro-1,3, 5-trinitro-1,3,5-triazine (RDX). The current pump and treat facility is preventing offsite migration but does not offer a short-term solution. Our objective was to quantify the effectiveness of permanganate to degrade RDX in situ. This was accomplished by performing laboratory treatability experiments, aquifer characterization, and a pilot-scale in situ chemical oxidation (ISCO) demonstration. Treatability experiments confirmed that permanganate could mineralize RDX in the presence of NOP aquifer solids. The pilot-scale ISCO demonstration was performed using an extraction-injection well configuration to create a curtain of permanganate between two injection wells. RDX destruction was then quantified as the RDX-permanganate plume migrated downgradient through a monitoring well field. Electrical resistivity imaging (ERI) was used to identify the subsurface distribution of permanganate after injection. Results showed that RDX concentrations temporally decreased in wells closest to the injection wells by 70% to 80%. Observed degradation rates (0.12 and 0.087/d) were lower than those observed under laboratory batch conditions at 11.5 ℃ (0.20/d) and resulted from lower than projected permanganate concentrations. Both ERI and spatial electrical conductivity measurements verified that permanganate distribution Was not uniform throughout the 6.1-m (20 feet) well screens and that groundwater sampling captured both treated and nontreated groundwater during pumping. Although heterogeneous flow paths precluded a uniform permanganate distribution, pilot-scale results provided proof-of-concept that permanganate can degrade RDX in situ and support permanganate as a possible remedial treatment for RDX-contaminated groundwater.
机译:前内布拉斯加军械厂(NOP)下的地下水被爆炸性六氢-1,3,5-三硝基-1,3,5-三嗪(RDX)污染。当前的泵送和处理设施可以防止异地迁移,但不能提供短期解决方案。我们的目标是量化高锰酸盐降解原位RDX的有效性。这是通过进行实验室可处理性实验,含水层表征和中试规模的原位化学氧化(ISCO)演示来实现的。可处理性实验证实,在存在NOP含水层固体的情况下,高锰酸盐可以使RDX矿化。使用提取注入井配置在两个注入井之间创建高锰酸盐帘幕,进行中试规模的ISCO演示。然后,随着RDX高锰酸盐羽流通过监测井场向下迁移,对RDX的破坏进行了量化。电阻率成像(ERI)用于识别注入后高锰酸盐的地下分布。结果表明,最接近注入井的井中RDX浓度随时间下降70%至80%。在11.5℃(0.20 / d)下观察到的降解速率(0.12和0.087 / d)低于实验室分批条件下观察到的降解速率,这是由于高锰酸盐浓度低于预期。 ERI和空间电导率测量结果都证明,高锰酸盐分布在整个6.1米(20英尺)的井网中并不均匀,并且在抽水过程中,地下水采样捕获了处理过的和未处理过的地下水。尽管异质流径排除了高锰酸盐的均匀分布,但中试规模的结果提供了概念证明,即高锰酸盐可以原位降解RDX并支持高锰酸盐作为对RDX污染的地下水的可能补救措施。

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  • 来源
    《Ground Water Monitoring & Remediation》 |2010年第3期|P.96-106|共11页
  • 作者单位

    CH2M HILL, 11301 Carmel Commons Blvd., Suite 304, Charlotte, NC 28226;

    University of Nebraska-Lincoln, 205 Kiesselbach, Lincoln, NE 68583-0915;

    Department of Geosciences at the University of Nebraska-Lincoln, NE 68588;

    School of Geology at Oklahoma State University University, Stillwater, OK 74078;

    School of Natural Resources at the University of Nebraska-Lincoln, Lincoln, NE 68583;

    Civil Engineering Department at the University of Nebraska-Lincoln, Lincoln, NE 68583;

    University of Nebraska's Water Sciences Laboratory, University of Nebraska-Lincoln, Lincoln, NE 68583;

    Aquifer Solutions, Inc., 29025A Upper Bear Creek Road, Evergreen, CO 80439;

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