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首页> 外文期刊>Journal of Contaminant Hydrology >Time series geophysical monitoring of permanganate injections and in situ chemical oxidation of PCE, OU1 area, Savage Superfund Site, Milford,NH, USA
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Time series geophysical monitoring of permanganate injections and in situ chemical oxidation of PCE, OU1 area, Savage Superfund Site, Milford,NH, USA

机译:美国新罕布什尔州萨维奇超级基金站点,高锰酸盐注射液的时间序列地球物理监测和PCE OU1区的原位化学氧化

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摘要

In situ chemical oxidation (ISCO) treatment with sodium permanganate, an electrically conductive oxidant, provides a strong electrical signal for tracking of injectate transport using time series geophysical surveys including direct current (DC) resistivity and electromagnetic (EM) methods. Effective remediation is dependent upon placing the oxidant in close contact with the contaminated aquifer. Therefore, monitoring tools that provide enhanced tracking capability of the injectate offer considerable benefit to guide subsequent ISCO injections. Time-series geophysical surveys were performed at a superfund site in New Hampshire, USA over a one-year period to identify temporal changes in the bulk electrical conductivity of a tetrachloroethylene (PCE; also called tetrachloroethene) contaminated, glacially deposited aquifer due to the injection of sodium permanganate. The ISCO treatment involved a series of pulse injections of sodium permanganate from multiple injection wells within a contained area of the aquifer. After the initial injection, the permanganate was allowed to disperse under ambient groundwater velocities. Time series geophysical surveys identified the downward sinking and pooling of the sodium permanganate atop of the underlying till or bedrock surface caused by density-driven flow, and the limited horizontal spread of the sodium permanganate in the shallow parts of the aquifer during this injection period. When coupled with conventional monitoring, the surveys allowed for an assessment of ISCO treatment effectiveness in targeting the PCE plume and helped target areas for subsequent treatment.
机译:使用高锰酸钠(一种导电氧化剂)进行的原位化学氧化(ISCO)处理可使用时间序列地球物理测量(包括直流(DC)电阻率和电磁(EM)方法)为跟踪注入传输提供强大的电信号。有效的补救措施取决于将氧化剂与受污染的含水层紧密接触。因此,提供增强的注射跟踪能力的监测工具可为指导后续的ISCO注射提供可观的收益。在一年的时间里,在美国新罕布什尔州的一家超级基金现场进行了时间序列地球物理调查,以确定注入造成的四氯乙烯(PCE;也称为四氯乙烯)受污染的冰川沉积含水层的整体电导率随时间的变化。高锰酸钠。 ISCO处理涉及从含水层封闭区域内的多个注入井中进行一系列高锰酸钠的脉冲注入。初始注入后,使高锰酸盐在环境地下水速度下分散。时间序列地球物理调查确定了由密度驱动的水流引起的下层耕作或基岩表面顶部的高锰酸钠向下沉陷和汇聚,以及在该注入期中高锰酸钠在含水层浅层中有限的水平扩散。结合常规监测,这些调查可以评估ISCO治疗针对PCE羽流的有效性,并帮助确定后续治疗区域。

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