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An Ensemble Level Upscaling Approach for Efficient Estimation of Fine-Scale Production Statistics Using Coarse-Scale Simulations

机译:使用粗尺度模拟有效估算精细生产统计数据的集成级别提升方法

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Upscaling is often needed in reservoir simulation to coarsen highly detailed geological descriptions. Most existing upscaling procedures aim to reproduce fine-scale results for a particular geological model (realization). In this work we develop and test a new approach, ensemble level upscaling, for efficiently generating upscaled two-phase flow parameters (e.g., upscaled relative permeabilities) for multiple geological realizations. For this purpose, flow-based upscaling calculations are combined with a statistical estimation procedure (cluster analysis). This approach allows us to numerically compute the upscaled two-phase flow functions for only a small portion of the coarse blocks. For the majority of blocks, these functions are estimated statistically based on single-phase velocity information (attributes), determined when the upscaled single-phase parameters are calculated. The procedure is designed to maintain close correspondence between the cumulative distribution functions for the numerically computed and statistically estimated two-phase flow functions. We apply the method to two-dimensional synthetic models of multiple realizations for uncertainty quantification. Models with different geological heterogeneity and fluid mobility ratios are considered. It is shown that the method consistently corrects the biases evident in primitive coarse-scale predictions and can capture the ensemble statistics (e.g., P50, P10, P90) of the fine-scale results almost as accurately as the full flow-based upscaling procedures, but with much less computational effort. The overall approach is flexible and can be used with any combination of upscaling procedures.
机译:在储层模拟中通常需要放大比例以粗化高度详细的地质描述。现有的大多数升级程序都旨在针对特定的地质模型(实现)再现精细的结果。在这项工作中,我们开发和测试了一种新的方法,即集成水平放大法,可以有效地生成用于多个地质实现的放大的两相流参数(例如,放大的相对渗透率)。为此,将基于流的放大计算与统计估计程序(集群分析)结合在一起。这种方法允许我们仅对一小部分粗块进行数值化的放大的两相流函数。对于大多数块,这些函数是根据单相速度信息(属性)进行统计估计的,这些信息是在计算出放大的单相参数时确定的。该程序旨在维护用于数字计算和统计估计的两相流函数的累积分布函数之间的紧密对应关系。我们将该方法应用于不确定性量化的多个实现的二维综合模型。考虑具有不同地质异质性和流体流动率的模型。结果表明,该方法可以始终如一地纠正原始粗尺度预测中明显的偏差,并且可以捕获细尺度结果的整体统计数据(例如P50,P10,P90),几乎与基于流的按比例放大过程一样准确,但所需的计算量却少得多。总体方法是灵活的,可以与升级过程的任何组合一起使用。

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