Bridging Computational Stratigraphy and Reservoir Simulation for Geologically Realistic High-Resolution Reservoir Modeling

Boxiao Li, Lewis Li, X. Wen, T. Sun
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引用次数: 1

Abstract

Computational Stratigraphy (CompStrat) is a state-of-the-art earth-modeling method that captures the key heterogeneities in subsurface reservoirs through modeling of the detailed flow and sediment transportation processes in various depositional environments. The method is fully based on physics and generates high-resolution 3D earth models that are much more geologically realistic than those generated by traditional earth-modeling methods. It can accurately predict and preserve those spatially continuous but vertically thin and volumetrically insignificant layers, such as shale layers, thus enabling a much more accurate representation of natural reservoir connectivity. In the past few years, CompStrat has been studied mainly within the earth science community and has yet been broadly applied in reservoir simulation research and practices. Our objective is to bridge this gap and allow this frontier technology to offer geologically realistic earth models for reservoir simulation to better understand how various geological features contribute and control subsurface flow patterns and performance, and subsequently leading to a better integration among earth modeling, flow simulation, and more reliable reservoir performance predictions. CompStrat models often have large number of cells (hundreds of millions or more). A large proportion of them are related to thin shale layers. These thin cells can often cause convergence difficulties in reservoir simulations. We developed a grid coarsening method to drastically reduce the cell number and the simulation time with minimum altering of overall model connectivity characteristics. The method reduces the cell number by 85% to 93% and the simulation time by 94% to 99.4% with limited loss of accuracy for representative examples. Without this method, the simulation may take impractically long time to run for large models with complex multiphase flow dynamics. The successful removal of the computational bottleneck enables the application of this frontier earth-modeling method in high-fidelity reservoir simulation. It also facilitates detailed understanding of the connection between geology and flow to offer valuable insight for reservoir modeling, production forecast uncertainty analysis, and history matching. We developed a method to label, evaluate, and rank geological features based on their influence on flow performance, with shale layers being the specific focus. The labeling is performed semi-automatically and the evaluation and ranking is done efficiently with a reduced-physics solver. The result is statistically consistent across multiple realizations.
桥接计算地层学和油藏模拟地质逼真的高分辨率油藏建模
计算地层学(CompStrat)是一种最先进的地球模拟方法,通过模拟各种沉积环境下的详细流动和沉积物运输过程,捕捉地下储层的关键非均质性。该方法完全基于物理,生成的高分辨率三维地球模型比传统地球建模方法生成的地质逼真得多。它可以准确地预测和保存那些空间上连续但垂直上薄且体积不显著的层,例如页岩层,从而能够更准确地表示天然储层的连通性。在过去的几年中,CompStrat主要在地球科学界进行研究,并已广泛应用于油藏模拟研究和实践中。我们的目标是弥合这一差距,并允许这一前沿技术为油藏模拟提供地质上真实的地球模型,以更好地了解各种地质特征如何影响和控制地下流动模式和性能,从而更好地将地球建模、流动模拟和更可靠的油藏性能预测结合起来。CompStrat模型通常有大量的单元格(数亿或更多)。其中很大一部分与薄页岩层有关。在油藏模拟中,这些薄单元通常会造成收敛困难。我们开发了一种网格粗化方法,在最小程度上改变模型整体连接特性的情况下,大大减少了单元数和模拟时间。该方法减少了85% ~ 93%的单元数,减少了94% ~ 99.4%的模拟时间,代表性示例的准确性损失有限。如果没有这种方法,对于具有复杂多相流动力学的大型模型,模拟可能需要很长时间才能运行。成功地消除了计算瓶颈,使该前沿地球模拟方法能够应用于高保真油藏模拟。它还有助于详细了解地质和流体之间的联系,为油藏建模、产量预测不确定性分析和历史匹配提供有价值的见解。我们开发了一种方法,根据地质特征对流动性能的影响对其进行标记、评估和排序,其中页岩层是重点。标记是半自动执行的,评估和排序是有效地完成与减少物理求解器。结果在统计上跨多个实现是一致的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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