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A new efficient averaging technique for scaleup of multimillion-cell geologic models

机译:一种新的高效平均技术,可扩展数百万个单元的地质模型

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Increased resolution in reservoir characterization is driving the need for efficient and accurate upscaling techniques for reservoir simulation on which reservoir performance prediction relies. Unfortunately, the existing averaging methods (i.e.harmonic, arithmetic, power law, geometric or a combination of harmonic and arithmetic methods) are only applicable under the circumstances of perfectly layered or perfectly random heterogeneity distributions, which realistic reservoirs are not. This paper presents a new averaging method that improves the upscaling averaging methods for realistic reservoirs and can substitute for the orders-of-magnitude slower performance of direct simulation methods, such as pressure solver techniques. The new averaging method first calculates the upper and lower bounds of the effective properties based on the nature of geology and then empolys a new correlation, scaling, and rotation technique to estimate the effective properties for the upscaled grid. The approach not only preserves the accuracy of the time consuming simulation methods but also retains the speed of the traditional averaging methods. Five real sandstone and carbonate reservoir geologic models (of which, three of them are multimillion cell models) from Africa, North America, and South America were employed as benchmark and working data sets to develop and validate the new technique. The technique has the advantage of suiting the more irregular geometries i.e. pinchouts, faults, and flexible simulation grids compared to the pressure solver methods which are more suited for relatively simple flow geometries.
机译:储层表征中分辨率的提高推动了对储层性能预测所依赖的储层模拟有效而准确的放大技术的需求。不幸的是,现有的平均方法(即谐波,算术,幂律,几何或谐波与算术方法的组合)仅适用于完全分层或完全随机的非均质分布的情况,而实际储集层则不适用。本文提出了一种新的平均方法,该方法改进了针对实际油藏的按比例放大平均方法,并且可以替代直接模拟方法(如压力求解器技术)的数量级较慢的性能。新的平均方法首先根据地质性质来计算有效属性的上限和下限,然后结合一种新的相关性,缩放和旋转技术来估计放大后的网格的有效属性。该方法不仅保留了费时的仿真方法的准确性,而且保留了传统平均方法的速度。来自非洲,北美和南美的五个真实的砂岩和碳酸盐岩储层地质模型(其中三个是数百万个单元模型)被用作开发和验证新技术的基准和工作数据集。与压力求解器方法相比,该技术具有更适合不规则几何形状(即,夹点,断层和灵活的模拟网格)的优势,而压力求解器方法更适合于相对简单的流动几何形状。

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