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Petroleum-hydrocarbon contamination and remediation by microbioventing at sub-Antarctic Macquarie Island

机译:亚南极麦格理岛的微生物排放对石油碳氢化合物的污染和修复

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Natural attenuation of petroleum hydrocarbons in polar and subpolar soils is limited by low nutrients, low temperatures, and water availability. This study investigated three sites contaminated with diesel fuel and the use of aeration to remediate one of the sites at sub-Antarctic Macquarie Island. These sites were of differing ages and had different soil-water regimes. The most recent spill (New Main Power House) occurred in 2002 and resulted in ~180 metric tons of highly-contaminated (~7000 mg kg~(-1)), moderately-drained, sandy soil. An older site (< 1994; Old Main Power House) comprised ~100 metric tons of moderately-contaminated (~2800 mg kg~(-1)) water-saturated peaty soil. A third spill (< 1994; Fuel Farm) contained approximately 600 metric tons of low- to moderately-contaminated (~800 mg kg~(-1)) sandy soil. Using a hydrocarbon distribution model (NAPLANAL) we determined that non-aqueous phase liquid droplets start to form in these soils at concentrations 50-1000 mg kg~(-1) mostly depending on organic carbon fraction. An in-field treatability evaluation with an air sparge port to increase oxygen concentration in the soils proved unsuccessful because the shallow water table and thin soil cover led to channel development. However, an easily-installed 'microbioventing' system, comprising many small air injecting rods, successfully aerated a wide area of soil. Field estimates of biodegradation rates under unamended aerobic conditions were ~10-20 mg kg~(-1) d~(-1). When considered with results from a nutrient optimisation respiration experiment [Walworth, J., Pond, A., Snape, I., Rayner, J.L. and Harvey, P.M., 2007-this issue. Nitrogen requirements for maximizing petroleum bioremediation in a sub-Antarctic soil. Cold Regions Science and Technology, In Press.], we conclude that in situ bioremediation for these sites should treat the soil to a target concentration of ~200 mg kg~(-1) in approximately 1-2 years of continual operation at ambient temperatures. This simple methodology could have useful application in the summer treatment of other waterlogged tundra soils.
机译:养分含量低,温度低和水利用率低,限制了极性和亚极性土壤中石油碳氢化合物的自然衰减。这项研究调查了三个被柴油污染的场所,并使用通气修复了南极麦格理岛附近的一个场所。这些地点年龄不同,土壤水情也不同。最近的一次泄漏(新主电厂)发生在2002年,造成〜180公吨高污染(〜7000 mg kg〜(-1)),中等排水的沙质土壤。较旧的场所(<1994年;旧的主要发电站)包含约100吨中度污染的(〜2800 mg kg〜(-1))水饱和的豌豆土。第三次泄漏(<1994年;燃料农场)包含大约600吨低污染至中度污染(〜800 mg kg〜(-1))的沙质土壤。使用碳氢化合物分布模型(NAPLANAL),我们确定非水相液滴开始在这些土壤中以50-1000 mg kg〜(-1)的浓度形成,这主要取决于有机碳含量。用空气喷射口提高土壤中氧浓度的现场可处理性评估未获成功,因为浅水位和薄薄的土壤覆盖物导致了河道发育。但是,一个易于安装的“微生物排放”系统(包括许多小型空气注入杆)成功地为大范围的土壤充气。在未经修正的有氧条件下,生物降解率的现场估算值为〜10-20 mg kg〜(-1)d〜(-1)。当考虑营养优化呼吸实验的结果时[Walworth,J.,Pond,A.,Snape,I.,Rayner,J.L.和Harvey,P.M.,2007-本期。在南极土壤中最大限度地利用石油进行生物修复的氮需求。 [Cold Regions Science and Technology,印刷中]。我们得出结论,这些位置的原位生物修复应在环境温度下连续运行约1-2年,将土壤处理至目标浓度约为〜200 mg kg〜(-1)。 。这种简单的方法可以在夏季处理其他涝渍苔原土壤中有用。

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