首页> 外文会议>International Symposium of the Society of Core Analysts >OIL RECOVERY IN THE TRANSITION ZONE OF CARBONATE RESERVOIRS WITH WETTABILITY CHANGE: HYSTERESIS MODELS OF RELATIVE PERMEABILITY VERSUS EXPERIMENTAL DATA
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OIL RECOVERY IN THE TRANSITION ZONE OF CARBONATE RESERVOIRS WITH WETTABILITY CHANGE: HYSTERESIS MODELS OF RELATIVE PERMEABILITY VERSUS EXPERIMENTAL DATA

机译:碳酸盐储层过渡区的储存带润湿性变化:相对渗透率与实验数据的滞后模型

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Due to its moderate permeability and/or very similar oil–water densities,the oil-water transition zone can extend over a large height and therefore contain a sizable amount of STOIIP. In the literature there is very scarce experimental data available for the oil-water system describing a drainage-imbibition process in the transition zone and practically none of them takes into account the variation of wettability on relative permeabilities. Most of the hysteresis models are based on simple extrapolations and do not incorporate wettability changes along the transition zone which is a key point especially in carbonate reservoirs. In a previous study [1] we performed steady-state core floods experiments with crude oil/brine on limestone cores over a large range of initial oil saturations and observed that wettability varies with height above the oil-water contact and has a strong impact on both oil and water imbibition relative permeabilities. Moreover we showed that there is no unique relationship between initial and residual oil saturations while the most used hysteresis models([2],[3],[4])are based on the same Land’s residual versus initial oil saturation relationship. The most sophisticated models incorporating wettability,such as Skjaeveland’s relative permeability hysteresis model [4] show better predictions but still need a lot of inputs that are not always available at laboratory scale. In this study,we compare our experimental data with the most used hysteresis models of relative permeability and we estimate the uncertainties on predicting oil recovery. We also present a new Kr hysteresis model,using the bounding Kr(relative permeability)curves and incorporating wettability change,which best fits our experimental data.
机译:由于其适度的渗透性和/或非常相似的油水密度,油水过渡区可以在大高度上延伸,因此含有大量的STOIIP。在文献中,对于在过渡区中描述排水 - 吸收过程的油水系统具有非常稀缺的实验数据,几乎没有考虑到相对渗透率的润湿性的变化。大多数滞后模型基于简单的外推,不包含沿着过渡区的润湿性变化,这是特别是在碳酸盐储层中的关键点。在先前的研究[1]中,我们在大型初始油饱和度上用原油/盐水进行了稳态核心洪水实验,并观察到润湿性随高于油水接触的高度而且产生强烈影响石油和水的吸收相对渗透率。此外,我们表明,初始和残留的油饱和性之间没有独特的关系,而最常用的磁滞模型([2],[3],[4])基于相同的土地的残留与初始油饱和关系。包含润湿性的最复杂的模型,例如Skjaevelang的相对渗透率滞后模型[4]显示更好的预测,但仍需要在实验室规模上不快提供许多输入。在本研究中,我们将我们的实验数据与相对渗透率最常用的磁滞模型进行比较,我们估计了预测储存的不确定性。我们还提供了一种新的KR滞后模型,使用边界KR(相对渗透率)曲线并包含润湿性变化,其最适合我们的实验数据。

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