786 research outputs found

    Electromagnetic imaging and deep learning for transition to renewable energies: a technology review

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    Electromagnetic imaging is a technique that has been employed and perfected to investigate the Earth subsurface over the past three decades. Besides the traditional geophysical surveys (e.g., hydrocarbon exploration, geological mapping), several new applications have appeared (e.g., characterization of geothermal energy reservoirs, capture and storage of carbon dioxide, water prospecting, and monitoring of hazardous-waste deposits). The development of new numerical schemes, algorithms, and easy access to supercomputers have supported innovation throughout the geo-electromagnetic community. In particular, deep learning solutions have taken electromagnetic imaging technology to a different level. These emerging deep learning tools have significantly contributed to data processing for enhanced electromagnetic imaging of the Earth. Herein, we review innovative electromagnetic imaging technologies and deep learning solutions and their role in better understanding useful resources for the energy transition path. To better understand this landscape, we describe the physics behind electromagnetic imaging, current trends in its numerical modeling, development of computational tools (traditional approaches and emerging deep learning schemes), and discuss some key applications for the energy transition. We focus on the need to explore all the alternatives of technologies and expertise transfer to propel the energy landscape forward. We hope this review may be useful for the entire geo-electromagnetic community and inspire and drive the further development of innovative electromagnetic imaging technologies to power a safer future based on energy sources.This work was supported by the European Union’s Horizon 2020 research and innovation programme under grant agreements No. 955606 (DEEP-SEA) and No. 777778 (MATHROCKS). Furthermore, the research leading of this study has received funding from the Ministerio de Educación y Ciencia (Spain) under Project TED2021-131882B-C42.Peer ReviewedPostprint (published version

    Electromagnetic imaging and deep learning for transition to renewable energies: a technology review

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    Electromagnetic imaging is a technique that has been employed and perfected to investigate the Earth subsurface over the past three decades. Besides the traditional geophysical surveys (e.g., hydrocarbon exploration, geological mapping), several new applications have appeared (e.g., characterization of geothermal energy reservoirs, capture and storage of carbon dioxide, water prospecting, and monitoring of hazardous-waste deposits). The development of new numerical schemes, algorithms, and easy access to supercomputers have supported innovation throughout the geo-electromagnetic community. In particular, deep learning solutions have taken electromagnetic imaging technology to a different level. These emerging deep learning tools have significantly contributed to data processing for enhanced electromagnetic imaging of the Earth. Herein, we review innovative electromagnetic imaging technologies and deep learning solutions and their role in better understanding useful resources for the energy transition path. To better understand this landscape, we describe the physics behind electromagnetic imaging, current trends in its numerical modeling, development of computational tools (traditional approaches and emerging deep learning schemes), and discuss some key applications for the energy transition. We focus on the need to explore all the alternatives of technologies and expertise transfer to propel the energy landscape forward. We hope this review may be useful for the entire geo-electromagnetic community and inspire and drive the further development of innovative electromagnetic imaging technologies to power a safer future based on energy sources

    HIBRIDNI ALGORITAM OPTIMIZACIJE ROJA ČESTICA I OPTIMIZACIJE SIVOGA VUKA ZA JEDNODIMENZIONALNO INVERZNO MODELIRANJE AUDIOFREKVENCIJSKE MAGNETOTELURIKE S KONTROLIRANIM IZVOROM (CSAMT)

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    The Controlled Source Audio-frequency Magnetotellurics (CSAMT) is a geophysical method utilizing artificial electromagnetic signal source to estimate subsurface resistivity structures. One-dimensional (1D) inversion modelling of CSAMT data is non-linear and the solution can be estimated by using global optimization algorithms. Particle Swarm Optimization (PSO) and Grey Wolf Optimizer (GWO) are well-known population-based algorithms having relatively simple mathematical formulation and implementation. Hybridization of PSO and GWO algorithms (called hybrid PSO-GWO) can improve the convergence capability to the global solution. This study applied the hybrid PSO-GWO algorithm for 1D CSAMT inversion modelling. Tests were conducted with synthetic CSAMT data associated with 3-layer, 4-layer and 5-layer earth models to determine the performance of the algorithm. The results show that the hybrid PSO-GWO algorithm has a good performance in obtaining the minimum misfit compared to the original PSO and GWO algorithms. The hybrid PSO-GWO algorithm was also applied to invert CSAMT field data for gold mineralization exploration in the Cibaliung area, Banten Province, Indonesia. The algorithm was able to reconstruct the resistivity model very well which is confirmed by the results from inversion of the data using standard 2D MT inversion software. The model also agrees well with the geological information of the study area.Audiofrekvencijska magnetotelurika s kontroliranim izvorom (CSAMT) geofizička je metoda koja se koristi izvorom umjetnoga elektromagnetskog signala za procjenu struktura otpornosti ispod površine. Jednodimenzionalno (1D) inverzno modeliranje CSAMT podataka nelinearno je te se rješenje može procijeniti korištenjem algoritama za globalnu optimizaciju. Algoritam roja čestica (PSO) i algoritam sivoga vuka (GWO) dobro su poznati algoritmi koji se temelje na populaciji i imaju relativno jednostavnu matematičku formulaciju i implementaciju. Hibridizacija PSO i GWO algoritama (hibridni PSO-GWO) može poboljšati sposobnost konvergencije prema globalnom rješenju. U ovom istraživanju primijenjen je hibridni PSO-GWO algoritam za 1D CSAMT inverzno modeliranje. Provedeno je testiranje sa sintetičkim CSAMT podatcima povezanim s 3-slojnim, 4-slojnim i 5-slojnim modelima zemlje kako bi se odredile performanse algoritma. Rezultati su pokazali kako hibridni PSO-GWO algoritam ima dobre performanse u postizanju minimalne neusklađenosti u usporedbi s originalnim PSO i GWO algoritmima. Hibridni PSO-GWO algoritam također je primijenjen za inverziju CSAMT terenskih podataka s ciljem istraživanja mineralizacije zlata u području Cibaliung, provincija Banten, Indonezija. Algoritam je uspio vrlo dobro rekonstruirati model otpornosti, što potvrđuju rezultati inverznoga modeliranja korištenjem standardnoga softvera za inverziju 2D magnetotelurskih podataka. Rezultati modela također se dobro podudaraju s geološkim informacijama istraživanoga područja

    Advances in Magnetotelluric Modelling: Time-Lapse Inversion, Bayesian Inversion and Machine Learning

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    This thesis presents advancements to the area of magnetotelluric (MT) modelling. There are three main aims to this work. The first aim is to implement an inversion to model time-lapse MT data in a temporal dimension. The algorithm considers the entire dataset at once, with penalisations for model roughness in both the spatial and temporal dimensions. The inversion is tested on synthetic data, as well as a case-study from a coal-seam gas dewatering survey. Second is to explore the problem of nonuniqueness in MT data inversion by implementing a 1D Bayesian inversion using an efficient sampler. The implemented model includes a novel way of regularising MT inversion by allowing the strength of smoothing to vary between different models. The Bayesian inversion is tested on synthetic and case-study datasets with results matching known data. The third aim is to implement a proxy function for the 3D MT forward function based on artificial neural networks. This allows for rapid evaluation of the forward function and the use of evolutionary algorithms to invert for resistivity structures. The evolutionary search algorithm is tested on synthetic data sets and a case-study data set from the Curnamona Province, South Australia. Together, these three novel algorithms and software implementations represent a contribution to the toolkit of MT modelling.Thesis (Ph.D.) -- University of Adelaide, School of Physical Sciences, 201

    Full Waveform Inversion Guided Wave Tomography Based on Recurrent Neural Network

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    Corrosion quantitative detection of plate or plate-like structures is a critical and challenging topic in industrial Non-Destructive Testing (NDT) research which determines the remaining life of material. Compared with other methods (X-ray, magnetic powder, eddy current), ultrasonic guided wave tomography has the advantages of non-invasiveness, high efficiency, high precision and low cost. Among various ultrasonic guided wave tomography algorithms, travel time or diffraction algorithms can be used to reconstruct defect or corrosion model, but the accuracy is low and heavily influenced by the noise. Full Waveform Inversion (FWI) can build accurate reconstructions of physical properties in plate structures, however, it requires a relatively accurate initial model, and there is still room for improvement in the convergence speed, imaging resolution and robustness. This thesis starting with the physical principle of ultrasonic guided waves, the dispersion characteristic curve of the guided wave propagating in the plate structure converts the change of the remaining thickness of the plate structure material into the wave velocity variation when the ultrasonic guided wave propagates in it, and provides a physical principle for obtaining the thickness distribution map from the velocity reconstruction. Secondly, a guided wave tomography method based on Recurrent Neural Network Full Waveform Inversion (RNN-FWI) is proposed. Finally, the efficiency of the above method is verified through practical experiments. The main work of the thesis includes: The feasibility of conventional full waveform inversion for guided wave tomography is introduced and verified. An FWI algorithm based on RNN is proposed. In the framework of RNN-FWI, the effects of different optimization algorithms on imaging performance and the effects of different sensor numbers and positions on imaging performance are analyzed. The quadratic Wasserstein distance is used as the objective equation to further reduce the dependence on the initial model. The depth image prior (DIP) based on convolutional neural network (CNN) is used as the regularization method to further improve the conventional FWI algorithm, and the effectiveness of the improved algorithm is verified by simulation and actual experiments

    Efficient Bayesian travel-time tomography with geologically-complex priors using sensitivity-informed polynomial chaos expansion and deep generative networks

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    Monte Carlo Markov Chain (MCMC) methods commonly confront two fundamental challenges: the accurate characterization of the prior distribution and the efficient evaluation of the likelihood. In the context of Bayesian studies on tomography, principal component analysis (PCA) can in some cases facilitate the straightforward definition of the prior distribution, while simultaneously enabling the implementation of accurate surrogate models based on polynomial chaos expansion (PCE) to replace computationally intensive full-physics forward solvers. When faced with scenarios where PCA does not offer a direct means of easily defining the prior distribution alternative methods like deep generative models (e.g., variational autoencoders (VAEs)), can be employed as viable options. However, accurately producing a surrogate capable of capturing the intricate non-linear relationship between the latent parameters of a VAE and the outputs of forward modeling presents a notable challenge. Indeed, while PCE models provide high accuracy when the input-output relationship can be effectively approximated by relatively low-degree multivariate polynomials, this condition is typically unmet when utilizing latent variables derived from deep generative models. In this contribution, we present a strategy that combines the excellent reconstruction performances of VAE in terms of prio representation with the accuracy of PCA-PCE surrogate modeling in the context of Bayesian ground penetrating radar (GPR) travel-time tomography. Within the MCMC process, the parametrization of the VAE is leveraged for prior exploration and sample proposal. Concurrently, modeling is conducted using PCE, which operates on either globally or locally defined principal components of the VAE samples under examination.Comment: 25 pages, 15 figure

    Advanced Geoscience Remote Sensing

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    Nowadays, advanced remote sensing technology plays tremendous roles to build a quantitative and comprehensive understanding of how the Earth system operates. The advanced remote sensing technology is also used widely to monitor and survey the natural disasters and man-made pollution. Besides, telecommunication is considered as precise advanced remote sensing technology tool. Indeed precise usages of remote sensing and telecommunication without a comprehensive understanding of mathematics and physics. This book has three parts (i) microwave remote sensing applications, (ii) nuclear, geophysics and telecommunication; and (iii) environment remote sensing investigations

    Inverse electromagnetic scattering models for sea ice

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    Journal ArticleInverse scattering algorithms for reconstructing the physical properties of sea ice from scattered electromagnetic field data are presented. The development of these algorithms has advanced the theory of remote sensing, particularly in the microwave region, and has the potential to form the basis for a new generation of techniques for recovering sea ice properties, such as ice thickness, a parameter of geophysical and climatological importance. Moreover, the analysis underlying the algorithms has led to significant advances in the mathematical theory of inverse problems
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