首页> 外文会议>SPE Abu Dhabi International Petroleum Exhibition Conference >Innovative Workflow for Grouping, Averaging, End-Point Scaling and Assessing Uncertainty of Water-Oil Relative-Permeability Curves, Considering Corresponding Normalized Water-Fractional-Flow Curves, Reservoir-Rock Types and Wettability Indexes
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Innovative Workflow for Grouping, Averaging, End-Point Scaling and Assessing Uncertainty of Water-Oil Relative-Permeability Curves, Considering Corresponding Normalized Water-Fractional-Flow Curves, Reservoir-Rock Types and Wettability Indexes

机译:考虑到相应的归一化水分流量曲线,水库 - 岩石类型和润湿性指标,用于分组,平均,终点缩放和评估水性相对渗透性曲线不确定性的创新工作流程

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Relative permeability is a key input for multiphase reservoir simulations. Challenges related to the validation and interpretation of the laboratory core measurements are associated with the restoration processes and resulting wettability states, the heterogeneities and multi-scale aspects of complex rocks, as well as the limitations of core flooding experiments. Moreover, the relative permeability curves from several samples can be scattered and their correlation with wettability and reservoir-rock types not directly apparent. Grouping, averaging, end-point scaling and assessing the data uncertainty are crucial steps in relative permeability data processing. To improve these processes, a new workflow is proposed, based on the water fractional flow concept (fw), which is an effective representation of the behavior of oil displacement by water injection, combining both relative permeability curves to oil and water into a single, equivalent curve. First, the water fractional flow curve, obtained from a relative permeability core flooding test, is normalized according to saturation end-points at a constant viscosity ratio equal to one. Such normalization allows the separation of the fw plot area into two regions according to the wettability state of the samples. Fractional flow curves for the same sample but at opposite wettability conditions, i.e. strongly oil-wet or water-wet, present a remarkable symmetry, from which a wettability index is calculated. This proposed new wettability index may then be compared to other indexes like Amott-Harvey or USBM for validation. Additionally, the shape of the normalized water fractional flow curves is influenced by rock-pore sizes. Subsequently, the normalized fractional flow curves are grouped by wettability and by reservoir-rock type, supporting the validation of the relative permeability data and identifying associated trends and uncertainties. The average, lower and upper-bound normalized fractional flow curves are obtained for each group. Likewise, relative-permeability and saturation end-points are correlated with reservoir-rock-type index or other rock properties. Finally, average, lower and upper-bound normalized relative permeability sets of curves and corresponding end-points may be used for reservoir simulation. Alternatively, de- normalized relative permeability curves can be obtained. By varying wettability, a controlled relative permeability dataset is obtained using direct-hydrodynamic (DHD) simulations on 3D digital rock model of a carbonate core sample. The proposed workflow is applied to such a dataset. The results confirm the ability of the method to correctly identify the different wetting states and to group the fractional flow curves accordingly. The proposed wettability index, directly obtained from relative permeability data, may be complementary to other industry wettability indexes and better represent the expected displacement behavior. The proposed workflow, although simple and widely applicable, considerably improves the relative permeability analysis process. It can be integrated with other core analysis, well-log analysis and digital-rock analysis workflows.
机译:相对渗透性是用于多相储层模拟的关键输入。与实验室核心测量的验证和解释有关的挑战与恢复过程和润湿性状态,复杂岩石的异质和多种方面以及核心泛滥实验的局限性相关。此外,来自几个样品的相对渗透性曲线可以分散,它们与润湿性和储层岩石类型的相关性不直接明显。分组,平均,终点缩放和评估数据不确定性是相对渗透性数据处理中的重要步骤。为了改进这些过程,基于水分流量概念(FW)提出了一种新的工作流程,这是通过注水的油位移行为的有效表示,将两个相对渗透率曲线与油和水相结合,进入单个,等价曲线。首先,从相对渗透性核心泛洪试验获得的水分数流动曲线根据恒定粘度比的饱和端点归一化。这种归一化允许根据样品的润湿性状态将FW绘图区域分离成两个区域。相同样品的分数流动曲线,但在相反的润湿性条件下,即强烈的油湿或水湿,呈现出一种显着的对称性,从中计算润湿性指数。然后可以将该提出的新润湿性指数与Amott-Harvey或USBM等其他指标进行比较。另外,归一化水分流量曲线的形状受到岩石孔径的影响。随后,归一化的分数流曲线通过润湿性和储存岩型分组,支持验证相对渗透性数据并识别相关趋势和不确定性。为每组获得平均,下部和上束的归一化分数流曲线。同样,相对渗透性和饱和端点与储层 - 岩型指数或其他岩石性能相关。最后,曲线和相应的端点的平均值,较低和上限归一化相对渗透集合可以用于储层模拟。或者,可以获得去归一化的相对渗透性曲线。通过改变润湿性,使用碳酸核核样品的3D数字岩体模型的直接水动力(DHD)模拟获得受控的相对渗透性数据集。所提出的工作流量适用于此类数据集。结果证实了该方法正确识别不同润湿状态的能力并相应地对分数流曲线进行分组。所提出的润湿性指数直接从相对渗透性数据获得,可能与其他行业润湿性指标互补,更好地代表预期的位移行为。拟议的工作流程虽然简单且广泛适用,大大提高了相对渗透性分析过程。它可以与其他核心分析,良好的日志分析和数字岩石分析工作流集成。

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