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Inversion using a new low-dimensional representation of complex binary geological media based on a deep neural network

机译:基于深度神经网络的复杂二元地质介质的新低维表示反演

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摘要

Efficient and high-fidelity prior sampling and inversion for complex geological media is still a largely unsolved challenge. Here, we use a deep neural network of the variational autoencoder type to construct a parametric low-dimensional base model parameterization of complex binary geological media. For inversion purposes, it has the attractive feature that random draws from an uncorrelated standard normal distribution yield model realizations with spatial characteristics that are in agreement with the training set. In comparison with the most commonly used parametric representations in probabilistic inversion, we find that our dimensionality reduction (DR) approach outperforms principle component analysis (PCA), optimization-PCA (OPCA) and discrete cosine transform (DCT) DR techniques for unconditional geostatistical simulation of a channelized prior model. For the considered examples, important compression ratios (200-500) are achieved. Given that the construction of our parameterization requires a training set of several tens of thousands of prior model realizations, our DR approach is more suited for probabilistic (or deterministic) inversion than for unconditional (or point-conditioned) geostatistical simulation. Probabilistic inversions of 2D steady-state and 3D transient hydraulic tomography data are used to demonstrate the DR-based inversion. For the 2D case study, the performance is superior compared to current state-of-the-art multiple-point statistics inversion by sequential geostatistical resampling (SGR). Inversion results for the 3D application are also encouraging.
机译:复杂地质介质的高效,高保真事先采样和反演仍然是一个尚未解决的挑战。在这里,我们使用变分自动编码器类型的深度神经网络来构造复杂的二进制地质介质的参数化低维基础模型参数化。为了进行反演,它具有吸引人的特征,即从具有与训练集一致的空间特征的不相关的标准正态分布产量模型实现中随机抽取。与概率反演中最常用的参数表示法相比,我们发现在无条件地统计模拟中,降维(DR)方法优于主成分分析(PCA),优化-PCA(OPCA)和离散余弦变换(DCT)DR技术通道化先验模型对于所考虑的示例,实现了重要的压缩比(200-500)。鉴于参数化的构造需要成千上万的先前模型实现的训练集,因此与无条件(或点条件)地统计模拟相比,我们的DR方法更适合于概率(或确定性)反演。 2D稳态和3D瞬态液压层析成像数据的概率反演用于证明基于DR的反演。对于2D案例研究,通过顺序地统计重采样(SGR),其性能优于当前最新的多点统计反演。 3D应用程序的反演结果也令人鼓舞。

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