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IMPROVING DIGITAL ROCK PHYSICS PREDICTIVE POTENTIAL FOR RELATIVE PERMEABILITIES FROM EQUIVALENT PORE NETWORKS

机译:从等效孔隙网络提高数字岩体物理预测潜力的相对渗透性

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Both single-phase and multiphase transport properties computed using quasi-static pore network models show sensitivities to the pore network extraction methods. Bondino et al. [1] show that differences do exist between predicted single-phase petrophysical properties and relative permeabilities for the same sample as a result of differences in the extracted pore networks from digital rock images. Idowu et al. [2] also show that differences do exist in predicted single-phase properties from different pore networks generated from the same sample. Using the same geometrical characterization, they [2] however, show that predicted multiphase transport properties from different pore networks are consistent if the topology of the pore space is well preserved in the extracted skeletons. In addition to the differences in the predicted transport properties, comparison of water-wet and oil-wet relative permeability trends from Bondino et al. [1] and Zhao et al. [3] show counter-intuitive trends for some of the pore networks. Using the same sample as Bondino et al. [1] and a quasi-static pore network model, we examine the causes of the apparent differences in the predicted multiphase transport properties and counter-intuitive relative permeability trends. In real porous media, there is no demarcation of the pore space volume to throats and pores but this is required in pore network models. We show that this geometrical characterization/partitioning of pore network elements in general have significant impacts on predicted single-phase and multiphase transport properties. For the networks examined in this study in particular, differences in the predicted single-phase and multiphase properties are caused mainly by the estimated lengths for pores and throats. However, volumes associated with (or allocated to) pores and throats during the pore network extraction processes are responsible for the observed counter-intuitive relative permeability trends.
机译:使用准静态孔径网络模型计算的单相和多相传输特性均显示对孔网络提取方法的敏感性。 Bondino等人。 [1]表明,由于来自数字岩图像中提取的孔网络的差异,在相同样本的预测单相岩石物理特性和相同渗透之间存在差异。念头等人。 [2]还表明,来自来自同一样本产生的不同孔网络的预测单相特性存在差异。使用相同的几何表征,它们[2]但是,如果孔隙空间的拓扑保存在提取的骨架中,则从不同孔网络中预测的多相传输性质是一致的。除了预测的运输特性的差异外,来自Bondino等人的水湿和油湿相对渗透率趋势的比较。 [1]和Zhao等人。 [3]显示一些孔隙网络的反向直观趋势。使用与BONDINO等相同的样品。 [1]和准静态孔隙网络模型,我们研究了预测的多相运输特性和反向直观相对渗透率趋势的表观差异的原因。在真正的多孔介质中,没有孔隙空间体积的划分到喉部和孔,但这是在孔网络模型中需要的。我们表明,这种几何表征/分区通常对预测的单相和多相传输性能产生显着影响。对于本研究中检查的网络,特别是预测单相和多相性能的差异主要是孔和喉部的估计长度引起的。然而,在孔网络提取过程中与(或分配给)孔隙和喉部相关的体积负责观察到的反向直观的相对渗透趋势。

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