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Evaluation of surface diffusion in microporous/mesoporous media using a numerical model applied to rate-of-adsorption data: Implications for improved gas permeability estimation in shales/tight rocks using drill cuttings

机译:使用应用对吸附率数据的数值模型评估微孔/中孔介质中的表面扩散:利用钻剪钻改善储岩/紧密岩石的改善气体渗透率估计的影响

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Adsorbed-phase surface diffusion has been recognized as an important controlling factor on gas apparent permeability in micropores and smaller mesopores. However, for the estimation of surface diffusion coefficients of shales, the commonly used empirical methods cannot account for the complexity of rock fabric in the matrix system of tight rocks. Further, the small sample sizes and amounts ( 5 g) of drill cuttings, which are usually the only reservoir samples available from horizontal wells, significantly limit the feasibility and reliability of current experimental methods for the direct quantification of surface diffusion coefficients. The primary objectives of this study are therefore to: 1) establish an integrated experimental and modeling approach to evaluate surface diffusion and permeability using drill cuttings, and 2) investigate the significance of surface diffusion in different adsorbate/adsorbent systems. In this work, a bidisperse numerical model is developed to extract surface diffusion coefficients and permeability/diffusivity values from porous materials by matching the pressure transient data recorded during gas adsorption. A high-resolution gas adsorption apparatus is employed to measure gas sorption kinetics under low-temperature (N-2, -196 degrees C; CO2, 0 degrees C), low-pressure ( 0.1 MPa) conditions, using small amounts ( 2 g) of powdered/crushed samples. The proposed model successfully matched rate-of-adsorption (ROA) pressure transient data on two synthetic micro/mesoporous materials (Activated Carbon and SBA-15) and five organic-rich shale samples. It was observed that surface diffusion is a dominant flow mechanism and enhances permeability/diffusivity in micropores and smaller mesopores. The new model improves upon the results of a previously-developed ROA model.
机译:吸附相表面扩散已被认为是微孔和较小的中孔中气体表观渗透性的重要控制因子。然而,为了估计Shales的表面扩散系数,常用的经验方法不能考虑岩织物在紧密岩石的矩阵系统中的复杂性。此外,小样本尺寸和量(<5g)的钻屑,通常是水平井的唯一可获得的储存器样本,显着限制了当前实验方法的直接定量表面扩散系数的可行性和可靠性。因此,本研究的主要目标是:1)建立一种综合的实验和建模方法来评估使用钻扦插的表面扩散和渗透率,2)研究表面扩散在不同吸附/吸附系统中的意义。在这项工作中,通过匹配在气体吸附期间记录的压力瞬态数据匹配来提取来自多孔材料的表面扩散系数和渗透率/扩散率值的平衡数值模型。使用少量测量低温(N-2,-196摄氏度C),低压(<0.1MPa)条件下测量气体吸附动力学的气体吸附动力学(< 2g)粉末/碎样品。所提出的模型成功匹配了两个合成微/介孔材料(活性炭和SBA-15)和五种有机富含物质样品的吸附率(ROA)压力瞬态数据。观察到表面扩散是主要的流动机制,并增强微孔中的渗透性/扩散性和更小的中孔。新模型提高了先前开发的ROA模型的结果。

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