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A numerical study on oxygen adsorption in porous media of coal rock based on fractal geometry

机译:基于分形几何的煤岩多孔介质中氧吸附的数值研究

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摘要

In order to explore the factors affecting coal spontaneous combustion, the fractal characteristics of coal samples are tested, and a pore-scale model for oxygen adsorption in coal porous media is developed based on self-similar fractal model. The liquid nitrogen adsorption experiments show that the coal samples indicate evident fractal scaling laws at both low-pressure and high-pressure sections, and the fractal dimensions, respectively, represent surface morphology and pore structure of coal rock. The pore-scale model has been validated by comparing with available experimental data and numerical simulation. The present numerical results indicate that the oxygen adsorption depends on both the pore structures and temperature of coal rock. The oxygen adsorption increases with increased porosity, fractal dimension and ratio of minimum to maximum pore sizes. The edge effect can be clearly seen near the cavity/pore, where the oxygen concentration is low. The correlation between the oxygen adsorption and temperature is found to obey Langmuir adsorption theory, and a new formula for oxygen adsorption and porosity is proposed. This study may help understanding the mechanisms of oxygen adsorption and accordingly provide guidelines to lower the risk of spontaneous combustion of coal.
机译:为了探索影响煤自燃的因素,测试了煤样品的分形特征,并基于自相似分形模型建立了煤多孔介质中氧吸附的孔尺度模型。液氮吸附实验表明,煤样在低压段和高压段均表现出明显的分形标度律,分形维数分别代表了煤岩的表面形态和孔隙结构。通过与可用的实验数据和数值模拟进行比较,对孔尺度模型进行了验证。目前的数值结果表明,氧的吸附取决于煤岩的孔隙结构和温度。氧吸附随着孔隙率,分形维数和最小孔径与最大孔径之比的增加而增加。在氧浓度低的腔/孔附近可以清楚地看到边缘效应。遵循朗缪尔(Langmuir)吸附理论,发现了氧的吸附与温度的关系,并提出了一个新的氧吸附与孔隙率的公式。这项研究可能有助于理解氧的吸附机理,从而为降低煤的自燃风险提供指导。

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