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Modeling discrete gas bubble formation and mobilization during subsurface heating of contaminated zones

机译:模拟受污染区域地下加热过程中离散的气泡形成和运动

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摘要

During thermal remediation the increase in subsurface temperature can lead to bubble formation and mobilization. In order to investigate the effect of gas formation on resulting aqueous concentrations, a 2D finite difference flow and mass transport model was developed which incorporates a macroscopic invasion percolation (MIP) model to simulate bubble expansion and movement. The model was used to simulate three soil scenarios with different permeabilities and entry pressures at various operating temperatures and groundwater velocities. It was observed that discrete bubble formation occurred in all three soils, upward mobility being limited by lower temperatures and higher entry pressures. Bubble mobilization resulted in a different aqueous mass distribution than if no discrete gas formation was modeled, especially at higher temperatures. This was a result of bubbles moving upwards to cooler areas, then collapsing, and contaminating previously clean zones. The cooling effect also led to possible non-aqueous phase liquid (NAPL) formation which was not predicted using a model without discrete bubble formation.
机译:在热修复过程中,地下温度的升高可能导致气泡形成和移动。为了研究气体形成对最终水浓度的影响,开发了二维有限差分流量和质量传输模型,该模型结合了宏观入侵渗滤(MIP)模型来模拟气泡的膨胀和运动。该模型用于模拟三种在不同工作温度和地下水速度下具有不同渗透率和入口压力的土壤情况。观察到,在所有三种土壤中均发生了离散的气泡形成,向上的流动性受到较低的温度和较高的进入压力的限制。与没有模拟离散气体形成的情况相比,气泡动员导致的水质分布有所不同,尤其是在较高温度下。这是由于气泡向上移动到较凉爽的区域,然后坍塌并污染了先前干净的区域的结果。冷却效果还导致可能形成非水相液体(NAPL),这是使用没有离散气泡形成的模型无法预测的。

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