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Modeling Mud-Filtrate Invasion Effects on Resistivity Logs to Estimate Permeability of Vuggy and Fractured Carbonate Formations

机译:泥浆滤液对电阻率的侵袭效应估算抗腐败和骨质碳酸酯的渗透性

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We develop and validate a new method to diagnose and estimate secondary porosity and absolute permeability of fractured and vuggy carbonate formations based on the numerical simulation of the process of mud-filtrate invasion. The method includes the geological characterization of core laboratory data and their integration with well logs and fluid production measurements. We apply the new method to the interpretation of data acquired in a carbonate reservoir in the Barinas-Apure Basin in southwest Venezuela. The latter reservoir behaves as a triple-porosity petrophysical system which exhibits inter-crystalline, intra-crystalline, moldic, vuggy (connected and non-connected) and fractured porosity, all embedded in a tight matrix. Rock-core data and wellbore resistivity images indicate that vugs are the mayor component of secondary porosity while fractures and interconnected vugs account for most of the permeability. The initial phase of our interpretation method consists of integrating core measurements with conventional and non-conventional well logs to calculate static and dynamic petrophysical properties via standard carbonate evaluation procedures. Starting with the calculated petrophysical properties, we simulate the process of invasion with both water- and oil-base muds. Resulting spatial distributions of water saturation and salt concentration in the near-borehole region give rise to spatial distributions of electrical resistivity which are used to numerically simulate laterolog and induction apparent resistivity logs. If the input values of porosity and permeability are not correct, the simulation of mud-filtrate invasion will result in a poor match of resistivity logs. In such cases, we update porosity and permeability until securing a good match between measurements and simulations. This procedure was tested on several key wells with and without core measurements, wellbore resistivity images, and well-testing measurements. We conclusively find that our final estimates of porosity and permeability are in good agreement with the properties of the global petrophysical system. Differences between porosity and permeability before and after simulation of the process of invasion are reliable indicators of presence and influence of vugs and/or fractures in the displacement of hydrocarbons by mud filtrate.
机译:我们开发和验证诊断和估计次生孔隙和基于泥浆滤液侵入的过程的数值模拟压裂和孔洞碳酸盐岩地层绝对渗透率的新方法。该方法包括核心实验室数据的地质特征及其与测井和流体生产测量一体化。我们运用新方法在委内瑞拉西南部在巴里纳斯 - 阿普雷盆地碳酸盐岩储层获得的数据的解释。后者贮存表现为表现出帧间结晶内,结晶,moldic,晶洞(连接和非连接的)和断裂孔隙的三孔隙度的岩石物理系统中,所有嵌入在紧矩阵。岩石核心数据和井筒电阻率图像表明,孔洞是次生孔隙的市长分量,而裂缝和孔洞互连占据大部分渗透性。我们的解释方法的初始阶段包括集成芯测量结果与常规和非常规测井到计算静态和通过标准碳酸盐评价程序动态岩石物理属性。与计算出的岩石物理性质出发,模拟出两种水和油基泥浆侵入的过程。所得在近井眼区域引起其用于数值模拟侧向测井和感应表观电阻率测井电阻率的空间分布的水饱和度和盐浓度的空间分布。如果孔隙度和渗透率的输入值不正确,泥浆滤液侵入的模拟会导致电阻率测井的差的匹配。在这种情况下,我们更新孔隙度和渗透率,直到确保测量和模拟之间的良好匹配。这个程序在几个关键井有和没有核心的测量,井眼电阻率成像,和良好的测试测量测试。我们得出结论发现,我们的孔隙度和渗透率的最终估计是在与全球岩石物理系统的性能一致。之前和侵袭的方法的模拟后的孔隙率和渗透性之间的差异是由泥浆滤液存在下和在烃的位移孔洞和/或裂缝的影响的可靠的指标。

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