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Complex geology estimation using the iterative adaptive Gaussian mixture filter

机译:使用迭代自适应高斯混合滤波器的复杂地质估计

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In the past years, multi-point geostatistical simulation (MPS) geo-models have been used successfully to create realistic geological instances (facies fields). However, the conditioning of such geological deposits to production data is still a challenge, especially when an assisted history matching (AHM) model based on Bayesian inversion is used. This is hampered when we deal with complex geometry and topology and when the number of the facies types is greater than two. The estimation of the facies field is carried out combining two components: a parameterization of the facies field and a AHM method. In this study, we extend a parameterization of the facies fields, defined in a multidimensional normalized space by drawing from a marginal conditional Gaussian distribution. This is a generalization of a parameterization used in a previous study for channelized reservoirs and can be used for any type of geological layouts of the prior (in the MPS case, the training image). The parameterization ensures that the updates are always facies realization. However, traditional history matching methods tend to either destroy this topological structure or collapse into a single realization giving an unrealistic description of the uncertainty. To improve this issue, the iterative adaptive Gaussian mixture (IAGM) has been used as AHM method with a maximum of three iterations for the case studies. The method is tested for a 2D reservoir model, where four facies types are present, of which one exhibits channelized geometry. The topology is complex because two of the facies types cannot be in contact with each other. After assimilation of the production data, the IAGM was able to reduce the prior uncertainty toward an ensemble with realistic geological structure, with a good data match and predictive capacity.
机译:在过去的几年中,多点地统计模拟(MPS)地理模型已成功用于创建现实的地质实例(相场)。然而,将这样的地质沉积物调节到生产数据仍然是一个挑战,特别是当使用基于贝叶斯反演的辅助历史匹配(AHM)模型时。当我们处理复杂的几何形状和拓扑以及相类型的数量大于两个时,这会受到阻碍。相场的估计是结合两个部分进行的:相场的参数化和AHM方法。在这项研究中,我们通过从边际条件高斯分布中绘制,扩展了在多维归一化空间中定义的相场的参数化。这是先前研究中用于渠道化储层的参数化的概括,可以用于先前的任何类型的地质布局(在MPS情况下为训练图像)。参数化确保更新始终是相实现的。但是,传统的历史匹配方法往往会破坏这种拓扑结构,或者崩溃为单个实现,从而给不确定性提供了不切实际的描述。为了改善这个问题,在案例研究中,迭代自适应高斯混合(IAGM)已被用作AHM方法,最多可进行三个迭代。该方法针对二维储层模型进行了测试,其中存在四种相类型,其中一种具有通道化的几何形状。拓扑结构很复杂,因为两种相类型无法相互接触。对生产数据进行同化后,IAGM能够减少具有实际地质结构,具有良好数据匹配和预测能力的集成的先验不确定性。

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