Spontaneous Imbibition and an Interface-Electrostatics-Based Model of the Transition Zone Thickness of Hydrocarbon Reservoirs and Their Theoretical Interpretations

M. Amadu, A. Miadonye
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Abstract

The transition zone (TZ) of hydrocarbon reservoirs is an integral part of the hydrocarbon pool which contains a substantial fraction of the deposit, particularly in carbonate petroleum systems. Consequently, knowledge of its thickness and petrophysical properties, viz. its pore size distribution and wettability characteristic, is critical to optimizing hydrocarbon production in this zone. Using classical formation evaluation techniques, the thickness of the transition zone has been estimated, using well logging methods including resistivity and Nuclear Magnetic Resonance, among others. While hydrocarbon fluids’ accumulation in petroleum reservoirs occurs due to the migration and displacement of originally water-filled potential structural and stratigraphic traps, the development of their TZ integrates petrophysical processes that combine spontaneous capillary imbibition and wettability phenomena. In the literature, wettability phenomena have been shown to also be governed by electrostatic phenomena. Therefore, given that reservoir rocks are aggregates of minerals with ionizable surface groups that facilitate the development of an electric double layer, a definite theoretical relationship between the TZ and electrostatic theory must be feasible. Accordingly, a theoretical approach to estimating the TZ thickness, using the electrostatic theory and based on the electric double layer theory, is attractive, but this is lacking in the literature. Herein, we fill the knowledge gap by using the interfacial electrostatic theory based on the fundamental tenets of the solution to the Poisson–Boltzmann mean field theory. Accordingly, we have used an existing model of capillary rise based on free energy concepts to derive a capillary rise equation that can be used to theoretically predict observations based on the TZ thickness of different reservoir rocks, using well-established formation evaluation methods. The novelty of our work stems from the ability of the model to theoretically and accurately predict the TZ thickness of the different lithostratigraphic units of hydrocarbon reservoirs, because of the experimental accessibility of its model parameters.
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油气藏过渡带厚度的自发浸润和基于界面-静电模型及其理论解释
碳氢化合物储层的过渡带(TZ)是碳氢化合物池不可分割的一部分,它包含了相当一部分的矿藏,尤其是在碳酸盐岩石油系统中。因此,了解过渡带的厚度和岩石物理特性,即孔径分布和润湿特性,对于优化过渡带的碳氢化合物生产至关重要。利用经典的地层评估技术,采用电阻率和核磁共振等测井方法估算过渡带的厚度。油气流体在石油储层中的积聚是由于原本充满水的潜在构造和地层陷阱的迁移和位移造成的,而油气流体过渡带的开发则综合了自发毛细管浸润和润湿现象的岩石物理过程。文献表明,润湿现象也受静电现象支配。因此,鉴于储层岩石是具有可电离表面基团的矿物集合体,这些表面基团有助于形成电双层,因此 TZ 与静电理论之间的明确理论关系必须是可行的。因此,利用静电理论并以电双层理论为基础来估算 TZ 厚度的理论方法很有吸引力,但文献中缺乏这方面的研究。在此,我们以泊松-波尔兹曼平均场理论解的基本原理为基础,利用界面静电理论填补了这一知识空白。因此,我们利用现有的基于自由能概念的毛细管上升模型,推导出了一个毛细管上升方程,该方程可用于利用成熟的地层评估方法,根据不同储层岩石的 TZ 厚度从理论上预测观测结果。我们工作的新颖之处在于,由于模型参数可通过实验获得,该模型能够从理论上准确预测油气储层不同岩性地层单元的 TZ 厚度。
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