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A mass balance approach to investigate arsenic cycling in a petroleum plume

机译:质量平衡方法研究石油羽流中砷的循环

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摘要

Natural attenuation of organic contaminants in groundwater can give rise to a series of complex biogeochemical reactions that release secondary contaminants to groundwater. In a crude oil contaminated aquifer, biodegradation of petroleum hydrocarbons is coupled with the reduction of ferric iron (Fe(III)) hydroxides in aquifer sediments. As a result, naturally occurring arsenic (As) adsorbed to Fe(III) hydroxides in the aquifer sediment is mobilized from sediment into groundwater. However, Fe(III) in sediment of other zones of the aquifer has the capacity to attenuate dissolved As via resorption. In order to better evaluate how long-term biodegradation coupled with Fe-reduction and As mobilization can redistribute As mass in contaminated aquifer, we quantified mass partitioning of Fe and As in the aquifer based on field observation data. Results show that Fe and As are spatially correlated in both groundwater and aquifer sediments. Mass partitioning calculations demonstrate that 99.9% of Fe and 99.5% of As are associated with aquifer sediment. The sediments act as both sources and sinks for As, depending on the redox conditions in the aquifer. Calculations reveal that at least 78% of the original As in sediment near the oil has been mobilized into groundwater over the 35-year lifespan of the plume. However, the calculations also show that only a small percentage of As (similar to 0.5%) remains in groundwater, due to resorption onto sediment. At the leading edge of the plume, where groundwater is suboxic, sediments sequester Fe and As, causing As to accumulate to concentrations 5.6 times greater than background concentrations. Current As sinks can serve as future sources of As as the plume evolves over time. The mass balance approach used in this study can be applied to As cycling in other aquifers where groundwater As results from biodegradation of an organic carbon point source coupled with Fe reduction. (C) 2017 Elsevier Ltd. All rights reserved.
机译:地下水中有机污染物的自然衰减会引起一系列复杂的生物地球化学反应,这些反应会将次级污染物释放到地下水中。在受原油污染的含水层中,石油烃的生物降解与含水层沉积物中氢氧化铁(Fe(III))氢氧化物的还原相结合。结果,吸附在含水层沉积物中氢氧化铁Fe(III)上的天然存在的砷(As)从沉积物中转移到地下水中。但是,含水层其他区域沉积物中的Fe(III)具有通过吸收来减弱溶解的As的能力。为了更好地评估长期生物降解结合铁还原和砷迁移可以如何在受污染的含水层中重新分配砷质量,我们根据现场观测数据对含水层中铁和砷的质量分配进行了量化。结果表明,Fe和As在地下水和含水层沉积物中均具有空间相关性。质量分配计算表明,99.9%的铁和99.5%的砷与含水层沉积物有关。根据含水层中的氧化还原条件,沉积物既可以作为砷的来源,也可以作为砷的吸收剂。计算表明,在烟羽的35年寿命中,至少有78%的原始As在石油附近的沉积物中被转移到了地下水中。但是,计算还表明,由于吸收到沉积物上,地下水中仅保留了少量的As(约0.5%)。在羽流的前沿(地下水是低氧的),沉积物螯合了Fe和As,导致As积累的浓度比背景浓度高5.6倍。随着羽流随着时间的推移,当前的砷汇可作为砷的未来来源。本研究中使用的质量平衡方法可以应用于其他含水层中的砷循环,其中地下水砷是有机碳点源的生物降解和铁还原的结果。 (C)2017 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2017年第2期|1351-1361|共11页
  • 作者单位

    Virginia Tech, Dept Geosci, 926 W Campus Dr, Blacksburg, VA 24061 USA;

    Virginia Tech, Dept Geosci, 926 W Campus Dr, Blacksburg, VA 24061 USA;

    US Geol Survey, 12201 Sunrise Valley Dr, Reston, VA 20192 USA;

    Univ Minnesota, Dept Earth Sci, 310 Pillsbury Dr SE, Minneapolis, MN 55455 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Arsenic; Iron; Petroleum; Biodegradation; Mass distribution;

    机译:砷;铁;石油;生物降解;质量分布;
  • 入库时间 2022-08-17 13:26:23

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