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Improved Interpretation of Electrical Resistivity Measurements in Mixed-Wet Rocks: An Experimental Core-Scale Application and Model Verification

机译:改进了混合湿岩中电阻率测量的解释:实验核心尺度应用和模型验证

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摘要

Interpretation of electrical resistivity measurements for assessing hydrocarbon saturation in mixed-wet and hydrocarbon-wet rocks often requires extensive recalibrations of resistivity models. In these conventional resistivity models, the impact of wettability is not reliably incorporated. Recently, we analytically derived a new resistivity model that incorporates parameters to account for wettability and complexity of pore structure. This new model requires experimental veri cation to enhance its applicability in core-and log-scale domains. In this paper we (1) experimentally quantify the influence of wettability on electrical resistivity measurements, (2) improved and verified our analytically derived resistivity model in rocks with different levels of wettability at different water saturations, and (3) demonstrated the physical meaning of the parameters related to wettability in the resistivity model. We altered the wettability of selected core samples from the same rock type. To prepare the core samples as mixed-wet, a surfactant solution was injected into the samples and then they were aged in decane. These approaches created a range of wettability states in the samples. To quantify the altered wettability of the samples, we used the combined USBM and Amott-Harvey method along with sessile drop contact angle measurements. Next, we used a centrifuge to vary the water saturation in the core samples. We then measured the electrical resistivity of each sample. Finally, we improved the recently introduced resistivity model and compared the estimates of resistivity index from the improved model against the experimentally measured resistivity indices.
机译:评估混合湿法和碳氢化合物岩石中的烃饱和度的电阻率测量通常需要广泛的电阻率模型的重新校正。在这些传统的电阻率模型中,不可靠地掺入润湿性的影响。最近,我们分析了一种新的电阻率模型,该模型包括参数来解释孔隙结构的润湿性和复杂性。该新模型需要实验验证,以提高其在核心和日志尺度域中的适用性。在本文中,我们(1)通过实验量化润湿性对电阻率测量的影响,(2)改进并验证了我们在不同水饱和度的不同润湿性水平的岩石中的分析导出电阻率模型,(3)证明了物理意义与电阻率模型中的润湿性相关的参数。我们改变了相同岩石类型所选核心样本的润湿性。为了制备作为混合湿的核心样品,将表面活性剂溶液注入样品中,然后在癸烷中老化。这些方法在样品中创建了一系列润湿性状态。为了量化样品的改变润湿性,我们使用组合的USBM和Amott-Harve方法以及柄落触点角度测量。接下来,我们使用离心机来改变核心样本中的水饱和度。然后我们测量每个样品的电阻率。最后,我们改进了最近引入的电阻率模型,并将改进模型与实验测量电阻率指数的电阻率指数的估计进行了比较。

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