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A core-scale reconstructing method for shale

机译:页岩岩心尺度重建方法

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摘要

Characterization of shale cores with low and anisotropic permeability is complicated, due to the presence of multiscale pore structure and thin layers, and defies conventional methods. To accurately reproduce the morphology of multiscale pore structure of the shale core, a novel core-scale reconstructing method is proposed to reconstruct 3D digital-experimental models by means of the combination of SEM, EDS images, nitrogen adsorption and pressure pulse decay experiment result. In this method, the multiscale and multicomponent reconstructing algorithm is introduced to build the representative multiscale model for each layer, which can describe the complex 3D structures of nano organic pores, micro-nano inorganic pores, micro slits and several typical minerals. Especially, to reproduce the realistic morphology for shale, the optimization algorithm based on simulated annealing algorithm uses the experimental data as constrain conditions to adjust and optimize the model for each layer. To describe the bedding characteristics of the shale core, bedding fractures are constructed by analysis of the mineral distribution in the interface of two layers, and then the representative models for different layers are integrated together to obtain the final core-scale digital-experimental model. Finally, the model is validated by computing its morphological and flow properties and comparing them with those of the actual 3D shale sample. This method provide a way for systematically and continuously describe the multiscale and anisotropic pore structure (from nm-cm) of the shale core, and will be helpful for understanding the quality of the shale reservoir.
机译:由于存在多尺度孔隙结构和薄层,具有低渗透率各向异性各向异性的页岩岩心的表征十分复杂,这与常规方法不符。为了准确再现页岩岩心多尺度孔隙结构的形态,提出了一种新颖的岩心尺度重构方法,结合SEM,EDS图像,氮气吸附和压力脉冲衰减实验结果,重构了3D数字实验模型。在这种方法中,引入了多尺度和多分量重建算法来为每一层建立代表性的多尺度模型,该模型可以描述纳米有机孔,微纳米无机孔,微缝和几种典型矿物的复杂3D结构。特别是为了再现页岩的真实形态,基于模拟退火算法的优化算法将实验数据作为约束条件来调整和优化每一层的模型。为了描述页岩岩心的层理特征,通过分析两层界面中的矿物分布来构造层理裂缝,然后将不同层的代表性模型整合在一起,以获得最终的岩心尺度数字实验模型。最后,通过计算其形态和流动特性并将其与实际3D页岩样品的形态和流动特性进行比较来验证该模型。该方法为系统,连续地描述页岩岩心的多尺度各向异性孔隙结构(从nm-cm)提供了一种方法,将有助于理解页岩储层的质量。

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