深部煤层封存CO2过程热−流−固−化相互作用机制数值模拟研究

    Numerical simulation study on thermo-hydro-mechanical-chemical interaction mechanism during CO2 storage in deep coal seams

    • 摘要: 为了研究煤层注入CO2后,多元气体、水以及煤岩间物理化学作用对于注CO2提高煤层气采收率(CO2-ECBM)工程的影响,基于二元气体竞争吸附、渗流扩散、气体溶解以及矿物溶解沉淀动力学特征,建立CO2-ECBM的热−流−固−化耦合模型;使用CMG-GEM进行数值模拟研究,分析不同耦合方式下,注入策略以及地下水环境对气体吸附量、渗透率和无机矿物组分溶解沉淀的影响。结果表明:热−流−固−化耦合模型更为准确描述了气体在深部煤层中的运移行为;CO2注入后发生竞争吸附,注入井周围渗透率迅速降低,未被影响区域略微增加;在压力作用下,CO2溶解在水中,地下水酸性增强,不同地下水环境下无机矿物溶解沉淀行为不同,尤其是碳酸盐矿物,如白云石,由于Mg2+存在抑制溶解,可能造成孔道堵塞降低驱替效率。

       

      Abstract: In order to study the effects of physical and chemical interactions between multiple gases, water and coal rock after CO2 injecting in coal seams on the CO2-injected enhanced coalbed methane recovery (CO2-ECBM) project, based on the dynamic characteristics of binary gas competitive adsorption, seepage diffusion, gas dissolution and mineral dissolution and precipitation, a thermo-hydro-mechanical-chemical coupling model of CO2-ECBM was established. CMG-GEM was used for numerical simulation study to analyze the effects of injection strategies and groundwater environment on gas adsorption capacity, permeability and dissolution and precipitation of inorganic mineral components under different coupling methods.The results show that the coupled thermo-hydro-mechanical-chemical model can describe the gas migration behavior in deep coal seams more accurately. After CO2 injection, competitive adsorption occurs, and the permeability around the injection well decreases rapidly, while the unaffected area increases slightly. Under the action of pressure, CO2 dissolves in water, increasing the acidity of groundwater. The dissolution and precipitation behavior of inorganic minerals in different groundwater environments is different, especially for carbonate minerals such as dolomite. Due to the inhibition of dissolution by Mg2+, pore blockage may be caused and displacement efficiency may be reduced.

       

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