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

机译:一种合奏级Upscaling方法,用于使用粗尺度模拟有效地估计微尺度生产统计数字

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摘要

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:水库模拟中通常需要升级以驯化高度详细的地质描述。大多数现有的升级程序旨在为特定地质模型(实现)重现细微结果。在这项工作中,我们开发和测试新方法,集合级Umpaling,用于有效地产生多个地质识别的升高的两相流参数(例如,升高的相对渗透率)。为此目的,基于流量的Upscaling计算与统计估计程序(聚类分析)组合。该方法允许我们在数值上仅计算粗块的一小部分的上部两相流函数。对于大多数块,这些功能基于单相速度信息(属性)统计地估计,当计算上升高的单相参数时确定。该过程旨在在数值计算和统计估计的两相流函数之间保持累积分布函数之间的密切对应。我们将该方法应用于多种实现的二维合成模型以进行不确定性量化。考虑具有不同地质异质性和流体迁移率比的模型。结果表明,该方法一致地校正原始粗糙度预测中明显的偏差,并且可以捕获微尺度结果的集合统计(例如,P50,P10,P90),几乎可以准确地作为基于全流量的Upscaling程序,但是计算努力越来越少。整体方法是灵活的,可以与任何Upscaling程序的组合一起使用。

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