Inverse analysis with variational autoencoders: a comparison of shallow and deep networks

IF 3.5
Hao Wu, Daniel O’Malley, John K. Golden, Velimir Vesselinov
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引用次数: 4

Abstract

Inverse problems are applied to determine unknown properties by matching observational data with a physical model that often takes many parameters as input. To overcome the underconstrained nature of inverse problems and achieve good performance, an approach is presented involving regularization with a technique known as a variational autoencoder (VAE), which is trained to map a high-dimensional parameter space with a complex structure to a low-dimensional latent space with a simple structure. We apply this approach to unconditioned realizations of the parameters (hetero-geneous hydraulic fields) for a hydrogeological inverse problem. Two types of hydraulic conductivity fields are used to evaluate the characterization for the different levels of heterogeneity complexity of the physical inputs. This approach keeps the computational cost of generating the training data low. The reason is unconditioned realizations neither rely on the observational data used to perform the inverse analysis nor require any groundwater flow model forward runs. In addition, this approach applies regularization on a low-dimensional latent space from the VAE and increases optimization efficiency through automatic differentiation. Furthermore, two different neural network (NN) structures are tested for their utility in using the VAE for inverse analysis. The performance of a deep, convolutional neural network strongly depends on the dimensionality of the latent space, which requires tuning. In contrast, a shallow, dense neural network provides consistently accurate characterization without tuning. Our approach evaluates the advantages of the shallow, dense neural network over the deep, convolutional one and enables future application to a wide range of inverse problems.
变分自编码器的逆分析:浅网络和深网络的比较
逆问题是通过将观测数据与通常以许多参数作为输入的物理模型相匹配来确定未知属性的问题。为了克服反问题的欠约束性质并获得良好的性能,提出了一种涉及正则化的方法,该方法使用一种称为变分自编码器(VAE)的技术,该技术可以将具有复杂结构的高维参数空间映射到具有简单结构的低维潜在空间。我们将这种方法应用于水文地质反问题参数(非均质水场)的无条件实现。使用两种类型的水力传导率场来评估物理输入的不同非均质复杂性水平的表征。这种方法使生成训练数据的计算成本很低。原因是无条件实现既不依赖于用于逆分析的观测数据,也不需要任何地下水流动模型的正演。此外,该方法对来自VAE的低维潜在空间进行正则化,并通过自动微分提高优化效率。此外,还测试了两种不同的神经网络结构在使用VAE进行逆分析方面的效用。深度卷积神经网络的性能强烈依赖于潜在空间的维度,这需要调整。相比之下,一个浅的、密集的神经网络提供了一致的、准确的特征,而不需要调整。我们的方法评估了浅层、密集神经网络相对于深层、卷积神经网络的优势,并使其能够在未来应用于广泛的逆问题。
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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