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Steady-State Relative Permeability Measurements of Tight and Shale Rocks Considering Capillary End Effect

机译:考虑毛细管末端效应的致密和页岩岩石稳态渗透率测量

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摘要

Relative permeability (k(r)) data are the key factors for describing the behaviour of the multi-phase flow in porous media. During the k(r) measurements of low-permeability rocks, high capillary pressure can cause a significant liquid hold-up at the core outlet. This liquid hold-up, which is known as capillary end effect (CEE), is the main difficulty for laboratory measurements of relative permeability (k(r)) for tight and shale rocks. In this paper, a novel method is proposed to correct the CEE during the steady-state relative permeability (SS-k(r)) measurements. The integrity of the proposed method is evaluated by a set of artificially generated data and the experimental SS-k(r) data of an Eagle Ford shale sample. It is shown that accurate k(r) data can be obtained using the proposed technique. This technique can be used to estimate reliable k(r) data without any saturation profile measurement equipment, such as CT scan or MRI.
机译:相对渗透率(k(r))数据是描述多孔介质中多相流行为的关键因素。在低渗透率岩石的k(r)测量中,较高的毛细管压力会导致岩心出口处的大量液体滞留。这种液体滞留现象被称为毛细管末端效应(CEE),是致密和页岩岩石相对渗透率(k(r))实验室测量的主要困难。在本文中,提出了一种在稳态相对磁导率(SS-k(r))测量期间校正CEE的新方法。建议的方法的完整性通过一组人工生成的数据和Eagle Ford页岩样品的实验SS-k(r)数据进行评估。结果表明,使用所提出的技术可以获得准确的k(r)数据。该技术可用于估计可靠的k(r)数据,而无需任何饱和度轮廓测量设备,例如CT扫描或MRI。

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