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Estimating In Situ Biodegradation Rates of Petroleum Hydrocarbons and Microbial Population Dynamics by Performing Single-Well Push-Pull Tests in a Fractured Bedrock Aquifer

机译:通过在破裂的基岩含水层中进行单井推挽试验估算石油烃的原位生物降解率和微生物种群动态

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摘要

The single-well push-pull test (SWPPT) was adapted to quantify in situ aerobic respiration and deni-trification rates and to assess microbial population dynamics in a petroleum-contaminated fractured bedrock aquifer. Among three test wells, significant dissolved oxygen (DO) consumption was observed only in one well, with average zero- and first-order rate coefficients of 0.32±0.63 and 7.07±13.85 mmolL~(-1) day~(-1), respectively. Of the four test wells, significant NO_3~- consumption was noted in three wells. The average zero- and first-order rate coefficients were 2.87±2.21 and 11.83± 7.99 mmolL~(-1) day~(-1), respectively. These results indicate that NO_3~- was more effectively consumed within this fractured bedrock aquifer. Significant DO or NO_3~- (electron acceptors (EAs)) consumption, the limited contribution of Fe(Ⅱ) to overall EAs consumption, the production of dissolved CO_2 during aerobic respiration and denitri-fication tests, and N_2O production strongly suggest that the EAs consumption was largely due to microbial ac-rfvity. Detection of Variovorax paradox, benzene-degrading culture, and 28 novel microbial species after the addition of O_2 or NO_3~- suggests that EA injection into a fractured rock aquifer may stimulate aerobic or denitrifying petroleum-degrading microbes. Therefore, SWPPT may be useful for quantifying in situ aerobic respiration and denitrification rates and for assessing microbial population dynamics in petroleum-contaminated fractured bedrock aquifers.
机译:单井推挽试验(SWPPT)适用于量化原位有氧呼吸和脱硝率,并评估受石油污染的裂缝性基岩含水层中的微生物种群动态。在三个测试井中,仅在一个井中观察到显着的溶解氧(DO)消耗,平均零阶和一级速率系数分别为0.32±0.63和7.07±13.85 mmolL〜(-1)天〜(-1),分别。在四口测试井中,三口井的NO_3〜-消耗量很大。平均零级和一级速率系数分别为2.87±2.21和11.83±7.99 mmolL〜(-1)天〜(-1)。这些结果表明,NO_3〜-在该裂隙基岩含水层中被更有效地消耗。大量的DO或NO_3〜-(电子受体(EA))消耗,Fe(Ⅱ)对整个EA消耗的贡献有限,有氧呼吸和反硝化试验中溶解的CO_2的产生以及N_2O的产生强烈表明EA消费主要是由于微生物的活动。在加入O_2或NO_3〜-后检测到Variovorax悖论,苯降解培养物和28种新微生物,这表明将EA注入破裂的含水层中可能会刺激需氧或反硝化的石油降解微生物。因此,SWPPT可用于量化原位有氧呼吸和反硝化速率,以及评估受石油污染的裂缝性基岩含水层中的微生物种群动态。

著录项

  • 来源
    《Water, Air, and Soil Pollution》 |2013年第2期|1364.1-1364.14|共14页
  • 作者单位

    Department of Environmental Engineering, Daejeon University (Former: Research Institute for Environmental Technology and Sustainable Development, Korea University, Seoul, South Korea), Daejeon, South Korea;

    Department of Environmental Engineering, Korea University, Choongnam, South Korea;

    SK Innovation Co. Ltd., Seoul, South Korea;

    National Institute of Environmental Research, Incheon, South Korea;

    Department of Environmental Engineering, Korea University, Choongnam, South Korea;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    push-pull test; toluene; biodegradation rate; fractured bedrock aquifer;

    机译:推挽测试甲苯;生物降解率基岩含水层破裂;

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