Stochastic electrical resistivity tomography with ensemble smoother and deep convolutional autoencoders

IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
M. Aleardi, A. Vinciguerra, E. Stucchi, A. Hojat
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引用次数: 0

Abstract

To reduce both the computational cost of probabilistic inversions and the ill-posedness of geophysical problems, model and data spaces can be reparameterized into low-dimensional domains where the inverse solution can be computed more efficiently. Among the many compression methods, deep learning algorithms based on deep generative models provide an efficient approach for model and data space reduction. We present a probabilistic electrical resistivity tomography inversion in which the data and model spaces are compressed through deep convolutional variational autoencoders, while the optimization procedure is driven by the ensemble smoother with multiple data assimilation, an iterative ensemble-based algorithm. This method iteratively updates an initial ensemble of models that are generated according to a previously defined prior model. The inversion outcome consists of the most likely solution and a set of realizations of the variables of interest from which the posterior uncertainties can be numerically evaluated. We test the method on synthetic data computed over a schematic subsurface model, and then we apply the inversion to field measurements. The model predictions and the uncertainty assessments provided by the presented approach are also compared with the results of a Markov Chain Monte Carlo sampling working in the compressed domains, a gradient-based algorithm and with the outcomes of an ensemble-based inversion running in the un-compressed spaces. A finite-element code constitutes the forward operator. Our experiments show that the implemented inversion provides most likely solutions and uncertainty quantifications comparable to those yielded by the ensemble-based inversion running in the full model and data spaces, and the Markov Chain Monte Carlo sampling, but with a significant reduction of the computational cost.
随机电阻率断层成像与集成平滑和深度卷积自编码器
为了降低概率反演的计算成本和地球物理问题的病态性,可以将模型和数据空间重新参数化到低维域,这样可以更有效地计算逆解。在众多压缩方法中,基于深度生成模型的深度学习算法为模型和数据空间约简提供了一种有效的方法。我们提出了一种概率电阻率层析反演方法,该方法通过深度卷积变分自编码器压缩数据和模型空间,而优化过程由基于多次数据同化的集成平滑器驱动,这是一种基于迭代集成的算法。该方法迭代地更新根据先前定义的先验模型生成的初始模型集合。反演结果由最可能的解和一组感兴趣的变量的实现组成,后验不确定性可以从这些变量中得到数值计算。我们在一个示意图地下模型上计算的合成数据上测试了该方法,然后我们将反演应用于现场测量。该方法提供的模型预测和不确定性评估也与压缩域中的马尔可夫链蒙特卡罗采样结果、基于梯度的算法以及在非压缩空间中运行的基于集合的反演结果进行了比较。有限元代码构成正向运算符。我们的实验表明,实现的反演提供了最可能的解决方案和不确定性量化,可与在完整模型和数据空间中运行的基于集合的反演以及马尔可夫链蒙特卡罗采样所产生的结果相比较,但显著降低了计算成本。
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来源期刊
Near Surface Geophysics
Near Surface Geophysics 地学-地球化学与地球物理
CiteScore
3.60
自引率
12.50%
发文量
42
审稿时长
6-12 weeks
期刊介绍: Near Surface Geophysics is an international journal for the publication of research and development in geophysics applied to near surface. It places emphasis on geological, hydrogeological, geotechnical, environmental, engineering, mining, archaeological, agricultural and other applications of geophysics as well as physical soil and rock properties. Geophysical and geoscientific case histories with innovative use of geophysical techniques are welcome, which may include improvements on instrumentation, measurements, data acquisition and processing, modelling, inversion, interpretation, project management and multidisciplinary use. The papers should also be understandable to those who use geophysical data but are not necessarily geophysicists.
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