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Gas Pressure Prediction Model for Carbon Dioxide Injection in a Large-Scale Coal Matrix Experiment

机译:大规模煤基质实验中二氧化碳注射气体压力预测模型

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Carbon dioxide injection, gas flow, and adsorption of CO2 in a coal matrix are modelled by a large-scale physical experiment. The process primarily comprises an increase in the gas pressure from an unsaturated to a saturated status during gas injection followed by a reduction in the gas pressure due to the adsorption of CO2 after the cessation of gas injection. We developed a straightforward and effective calibration-based gas pressure model for the spatio-temporal prediction of CO2 in a coal matrix. The Nash-Sutcliffe efficiency of the models for predicting gas pressure is between 0.931 and 0.998. The results indicate that the spatio-temporal distribution of gas pressure in the coal matrix mainly relates to the gas pressure injected, geological boundary conditions, initial geo-stress, and gas type. The gas concentration tends to increase in high Earth stress and boundary areas during gas injection, whereas the gas adsorption rate is high in areas of low Earth stress. The gas adsorption rate of the coal matrix decreases as the gas injection content and gas injection time increase; improvement of the gas injection pressure can boost the gas adsorption to some extent. This model can explain or predict the behaviour of gas in a coal matrix depending on the matrix density, and it has the potential to simulate gas behaviour in a large-scale undisturbed coal sample considering the structure (joints and cleats) of the coal.
机译:二氧化碳注射,气体流动和煤基质中的二氧化碳和吸附是由大规模物理实验的建模。该过程主要包括在气体喷射期间从不饱和至饱和状态的气体压力的增加,然后由于CO 2的吸附在气体喷射后的吸附而降低气体压力。我们开发了一种直接且有效的基于校准的基于校准的气体压力模型,用于煤基质中CO2的时空预测。用于预测气体压力的模型的纳什Sutcliffe效率在0.931和0.998之间。结果表明,煤基质中气体压力的时空分布主要涉及注入的气体压力,地质边界条件,初始地理应力和气体类型。气体浓度趋于增加气体注射过程中的高地应力和边界区域,而气体吸附速率在低地球应激区域的区域高。煤基质的气体吸附速率随着气体注射含量和气体喷射时间增加而降低;气体注入压力的改善可以在一定程度上提高气体吸附。该模型可以根据基质密度来解释或预测煤基质中的气体的行为,并且考虑到煤的结构(接头和夹层),它具有模拟大规模未受干扰的煤样中的气体行为。

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