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A New Differentiable Parameterization Based on Principal Component Analysis for the Low-Dimensional Representation of Complex Geological Models

机译:基于主成分分析的复杂地质模型低维表示的一种新的可微分参数化

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A new approach based on principal component analysis (PCA) for the representation of complex geological models in terms of a small number of parameters is presented. The basis matrix required by the method is constructed from a set of prior geological realizations generated using a geostatistical algorithm. Unlike standard PCA-based methods, in which the high-dimensional model is constructed from a (small) set of parameters by simply performing a multiplication using the basis matrix, in this method the mapping is formulated as an optimization problem. This enables the inclusion of bound constraints and regularization, which are shown to be useful for capturing highly connected geological features and binary/bimodal (rather than Gaussian) property distributions. The approach, referred to as optimization-based PCA (O-PCA), is applied here mainly for binary-facies systems, in which case the requisite optimization problem is separable and convex. The analytical solution of the optimization problem, as well as the derivative of the model with respect to the parameters, is obtained analytically. It is shown that the O-PCA mapping can also be viewed as a post-processing of the standard PCA model. The O-PCA procedure is applied both to generate new (random) realizations and for gradient-based history matching. For the latter, two- and three-dimensional systems, involving channelized and deltaic-fan geological models, are considered. The O-PCA method is shown to perform very well for these history matching problems, and to provide models that capture the key sand–sand and sand–shale connectivities evident in the true model. Finally, the approach is extended to generate bimodal systems in which the properties of both facies are characterized by Gaussian distributions. MATLAB code with the O-PCA implementation, and examples demonstrating its use are provided online as Supplementary Materials.
机译:提出了一种基于主成分分析(PCA)的用少量参数表示复杂地质模型的新方法。该方法所需的基础矩阵由使用地统计算法生成的一组先验地质实现构造而成。与基于标准PCA的方法不同,在该方法中,仅通过使用基本矩阵执行乘法就可以从(少量)参数集构建高维模型,而在这种方法中,映射被公式化为优化问题。这样就可以包含约束和正则化约束,这对于捕获高度关联的地质特征和二元/双峰(而不是高斯)属性分布非常有用。这种方法被称为基于优化的PCA(O-PCA),在此主要应用于二进制相系统,在这种情况下,必要的优化问题是可分离的和凸的。通过分析获得优化问题的解析解以及模型相对于参数的导数。结果表明,O-PCA映射也可以看作是标准PCA模型的后处理。 O-PCA过程既用于生成新的(随机)实现,又用于基于梯度的历史匹配。对于后者,考虑了二维和三维系统,涉及通道化和三角扇形地质模型。 O-PCA方法在解决这些历史匹配问题方面表现出色,并提供了捕获真实模型中明显的关键砂-砂和砂-页岩连通性的模型。最后,该方法被扩展为生成双峰系统,其中两个相的性质都以高斯分布为特征。在线提供了作为补充材料的带有O-PCA实现的MATLAB代码以及演示其用法的示例。

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