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模拟乳化植物油反应区用于铬 (VI) 污染含水层的长期修复:地质参数和地下水微生物群落的动态演化。

Simulated reactive zone with emulsified vegetable oil for the long-term remediation of Cr(VI)-contaminated aquifer: dynamic evolution of geological parameters and groundwater microbial community.

机构信息

Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun, 130021, China.

出版信息

Environ Sci Pollut Res Int. 2018 Dec;25(34):34392-34402. doi: 10.1007/s11356-018-3386-z. Epub 2018 Oct 10.

Abstract

Cr(VI), which is highly toxic and soluble, is one of the most challenging groundwater contaminants. Previous work has indicated that emulsified vegetable oil (EVO) is an effective in situ amendment for removing Cr(VI) from groundwater. However, the spatial and temporal changes in geological parameters and microbial community structures throughout the remediation period are poorly understood. In this study, a large laboratory-scale sand-packed chamber (reactive zone of 100 × 50 × 30 cm) was used to simulate the bioremediation of Cr(VI)-contaminated aquifer by EVO over a 512-day period. Various geological parameters and microbial communities were monitored during both the establishment and remediation stages. The results indicate that several biogeochemical reactions occurred in a specific sequence following the injection of EVO, creating an acidic and reducing environment. A shift in the community structure and a decrease in the community diversity were observed. The abundance of microbes involved in the degradation of EVO and reduction of electron acceptors significantly increased. Then, the EVO reactive zone was flushed with Cr(VI)-contaminated groundwater. Biogeochemical reactions were inhibited after the inflow of Cr(VI) and subsequently recovered a month later. The pH of the aquifer returned to the initial neutral condition (approximately 7.2). The EVO reactive zone could remediate Cr(VI)-contaminated groundwater at an efficiency exceeding 97% over 480 days. Biogeochemistry played a major role in the early period (075 days). In the later period (240480 days), the remediation of Cr(VI) in the reactive zone depended mostly on bio-reduction by Cr(VI)-reducing bacteria.

摘要

六价铬(Cr(VI))具有高毒性和可溶性,是最具挑战性的地下水污染物之一。以前的工作表明,乳化植物油(EVO)是一种从地下水中去除 Cr(VI) 的有效原位修复剂。然而,在修复期间,地质参数和微生物群落结构的时空变化仍知之甚少。在这项研究中,使用大型实验室规模的砂填充室(反应区为 100×50×30 厘米)模拟了 EVO 对受 Cr(VI)污染的含水层进行生物修复的过程,历时 512 天。在建立和修复阶段监测了各种地质参数和微生物群落。结果表明,在注入 EVO 后,会按特定顺序发生几种生物地球化学反应,从而形成酸性和还原环境。群落结构发生了转变,群落多样性也有所下降。参与 EVO 降解和电子受体还原的微生物丰度显著增加。然后,用受 Cr(VI)污染的地下水冲洗 EVO 反应区。在 Cr(VI)流入后,生物地球化学反应受到抑制,一个月后恢复。含水层的 pH 值恢复到初始中性条件(约 7.2)。在 480 天内,EVO 反应区可以将 Cr(VI)污染的地下水的去除效率提高到 97%以上。生物地球化学在早期(075 天)起主要作用。在后期(240480 天),反应区中 Cr(VI)的修复主要依赖于 Cr(VI)还原菌的生物还原。

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