A Review of Seismic Full Waveform Inversion Based on Deep Learning

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초록

Full waveform inversion (FWI) in the field of seismic data processing is an inversion technique that is used to estimate the velocity model of the subsurface for oil and gas exploration. Recently, deep learning (DL) technology has been increasingly used for seismic data processing, and its combination with FWI has attracted remarkable research efforts. For example, DL-based data processing techniques have been utilized for preprocessing input data for FWI, enabling the direct implementation of FWI through DL technology. DL-based FWI can be divided into the following methods: pure data-based, physics-based neural network, encoder-decoder, reparameterized FWI, and physics-informed neural network. In this review, we describe the theory and characteristics of the methods by systematizing them in the order of advancements. In the early days of DL-based FWI, the DL model predicted the velocity model by preparing a large training data set to adopt faithfully the basic principles of data science and apply a pure data-based prediction model. The current research trend is to supplement the shortcomings of the pure data-based approach using the loss function consisting of seismic data or physical information from the wave equation itself in deep neural networks. Based on these developments, DL-based FWI has evolved to not require a large amount of learning data, alleviating the cycle-skipping problem, which is an intrinsic limitation of FWI, and reducing computation times dramatically. The value of DL-based FWI is expected to increase continually in the processing of seismic data.

키워드

full waveform inversiondeep learningreparameterizationphysics-informed neural networkMULTILAYER FEEDFORWARD NETWORKSCONVOLUTIONAL NEURAL-NETWORKOPTIMAL TRANSPORTVELOCITY ANALYSISFREQUENCY-DOMAINREFLECTION DATAPART 1REGULARIZATION
제목
A Review of Seismic Full Waveform Inversion Based on Deep Learning
저자
Pyun, SukjoonPark, Yunhui
DOI
10.7582/GGE.2022.25.4.227
발행일
2022
유형
Review
저널명
지구물리와 물리탐사
25
4
페이지
227 ~ 241