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Water and Oil Relative Permeability of Middle Bakken Formation: Experiments and Numerical Modeling

机译:中间Bakken形成的水和油相对渗透性:实验和数值模拟

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Relative permeability is one of the most important input function for reservoir modeling, production forecasting, and enhanced oil recovery calculations. The routine experimental methods to measure relative permeability are not adequate for very tight formations because of the long duration of experimental time and nonuniform saturation distribution in the core. The steady-state and unsteady-state measurements are the two common methods to measure relative permeability in conventional reservoir cores. In this paper, to measure water and oil relative permeability in unconventional core plugs from the Middle Bakken, we adopted a hybrid technique by Ramakrishnan and Cappiello (1991) which was designed to measure the non-wetting phase relative permeability in water-wet cores. Specifically, first we measured the relative permeability end-points for oil and water phases. Second, we used numerical modeling to calculate the entire relative permeability curves while honoring the measured end-point values. Relative permeability endpoints of water and oil at residual saturations were measured in one preserved and one cleaned Middle Bakken cores to establish credibility of the method. Then, these relative permeability endpoints were used as input to a numerical model of the Buckley-Leverett equation which included capillary end effects, to determine saturation distribution in both cores. Via history matching we obtained the relative permeability curve exponents. In this paper, we present the details of the experimental procedure and the data relevant to the Middle Bakken cores. We observed that the preserved oil-wet Bakken core imbibed the displacing synthetic brine solution which is contrary to the established wettability concept. We believe that the brine imbibition resulted from salinity contrast and chemical osmosis mass transfer across the inlet surface of the core.
机译:相对磁导率是储层建模,生产预测和强化油采收的计算的最重要的输入功能中的一个。在常规实验的方法来测量相对渗透率是不够的,因为实验时间和核心不均匀的饱和度分布的持续时间长的非常致密地层。稳态和非稳态测量是测量常规储层岩心相对渗透率的两种常见方法。在本文中,以测量水和油的相对渗透率在来自中东巴肯非常规芯插头,我们通过将其设计用于测量在水润湿芯中的非润湿相相对渗透率莱玛克里斯南和Cappiello(1991)的混合技术。具体而言,首先我们测量相对渗透率端点为油相和水相。第二,我们使用数值模拟来计算整个相对渗透率曲线同时遵从所测量的终点值。在一个保存,测定在残余饱和度的水和油的相对渗透率端点和一个清洁中间巴肯芯建立的方法的可信性。然后,这些相对渗透率端点被用作输入到其中包括毛细管末端效应巴克利 - 莱弗里特方程的数值模型,以确定在两个核饱和度分布。通过历史拟合,我们得到的相对渗透率曲线指数。在本文中,我们目前的实验程序的有关中东巴肯核心细节和数据。我们观察到,保留油湿巴肯核心吸入的置换合成盐水的解决方案,这是违反既定的润湿性的概念。我们认为,盐水吸造成的盐度差和整个核心的入口表面化学渗透传质。

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