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Simulation of oil spill infiltration and redistribution in a shallow aquifer

机译:浅层含水层中溢油渗透和再分布的模拟

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Simulations of oil spill infiltration and redistribution in a shallow aquifer were conducted in this work to quantify their effects on groundwater. Results showed that flow of oil spills can be adequately described by infiltration and redistribution patterns within the domain. Without the influence of rainfall, the contaminant plume pervaded the water table within one year of the spill through the influence of dissolution, diffusive and convective mechanisms. The plume advanced in the domain first by domain wall trailing in a manner suggestive of oil-wetting characteristics followed by bulk plume movement. Simultaneous infiltration with rainfall increased the rate of contaminant penetration and aided the plume front further into the domain. Without influence of rain, uncontaminated water can be found at a depth beyond 30 m from the spill surface at 30 years after the spill, while the possibility of clean water with influence of rainfall, at the same period of time, became remote even up to the bottom of the aquifer as the rainfall drives the plume into the furthest depth though, this is accompanied by cleaner water body at the upper portion of the aquifer. It was found that the impacts of contaminants on aquifer water are influenced by contaminant components, wettability of the aquifer, annual rates of rainfall, boundary conditions of the source and possibly size of the domain. Findings in this report point to the needs for quicker clean up exercises and identification of multi-approach procedures for different spill scenarios.
机译:在这项工作中,对溢油在浅层含水层中的渗透和重新分布进行了模拟,以量化其对地下水的影响。结果表明,可以通过域内的渗透和重新分布模式来充分描述漏油事件。在没有降雨影响的情况下,污染物羽流通过溶解,扩散和对流机制的影响在溢出的一年之内遍及了地下水位。羽流首先通过畴壁拖尾以暗示油润湿特征的方式前进,随后是散羽运动。降雨的同时渗透增加了污染物的渗透速度,并帮助羽流进一步进入了该区域。在不受雨水影响的情况下,在泄漏发生30年后,可以在距泄漏表面30 m以上的深度发现未受污染的水,而在同一时间段内,受到降雨影响的清洁水的可能性甚至很小。尽管降雨将羽流带入最深的深度,但在含水层的底部,这伴随着含水层上部较干净的水体。发现污染物对含水层水的影响受污染物成分,含水层的润湿性,年降雨率,水源边界条件以及可能的域大小影响。本报告中的发现表明需要针对不同的泄漏场景进行更快的清理工作并确定多方法程序。

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