An empirical study of large-scale data-driven full waveform inversion
Peng Jin1,2, Yinan Feng3, Shihang Feng3
1Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, USA. pqj5125@psu.edu.
Scientific Reports
|August 28, 2024
Summary
Big data significantly enhances deep learning models for seismic full waveform inversion (FWI). Training on large, diverse datasets improves accuracy and generalization, showing that model capacity must scale with data size for optimal results.
Area of Science:
- Geophysics
- Machine Learning
- Data Science
Background:
- Deep learning models show promise for solving complex geophysical problems like full waveform inversion (FWI).
- The impact of large-scale, diverse datasets on deep learning for FWI remains under-explored.
- OPENFWI provides a valuable resource for investigating big data's role in FWI.
Purpose of the Study:
- To empirically evaluate the effect of big data on deep learning models applied to the FWI problem.
- To quantify performance improvements in FWI using large, multi-structural synthetic datasets.
- To determine the relationship between model capacity and dataset size for optimal FWI performance.
Main Methods:
- Deep learning models were trained and evaluated on 10 2D subsets of the OPENFWI dataset, totaling 470,000 seismic data and velocity map pairs.
- Performance was assessed using Mean Absolute Error (MAE), Mean Squared Error (MSE), and Structural Similarity Index (SSIM).
- Experiments included comparisons between training on combined datasets versus individual subsets and leave-one-out generalization tests, alongside varying model capacities.
Main Results:
- Training on the combined OPENFWI dataset improved MAE by 13.03%, MSE by 7.19%, and SSIM by 1.87% compared to split datasets.
- Leave-one-out generalization tests showed average improvements of 28.60% in MAE, 21.55% in MSE, and 8.22% in SSIM.
- Increasing model capacity alongside data size yielded significant performance gains, with the largest model outperforming the smallest by 20.06% (MAE), 13.39% (MSE), and 0.72% (SSIM).
Conclusions:
- Big data, particularly large and diverse synthetic datasets like OPENFWI, demonstrably enhances deep learning model performance for full waveform inversion.
- Optimal performance in data-driven FWI requires a synergistic scaling of model capacity with the size and complexity of the training dataset.
- This study validates the effectiveness of big data in improving FWI accuracy and generalization, paving the way for more robust geophysical subsurface imaging.
Related Concept Videos
Basic Operations on Signals
Basic signal operations include time reversal, time scaling, time shifting, and amplitude transformations. These operations are fundamental in signal processing and analysis.
Time Reversal mirrors a continuous-time signal about the vertical axis at t=0. This is achieved by substituting t with −t. For example, if a signal x(t) is considered, the time-reversed signal is x(−t). This operation can be graphically represented, showing the mirrored signal.
Time Reversal mirrors a continuous-time signal about the vertical axis at t=0. This is achieved by substituting t with −t. For example, if a signal x(t) is considered, the time-reversed signal is x(−t). This operation can be graphically represented, showing the mirrored signal.
Deconvolution
Deconvolution, also known as inverse filtering, is the process of extracting the impulse response from known input and output signals. This technique is vital in scenarios where the system's characteristics are unknown, and they must be inferred from the observable signals.
Deconvolution involves several mathematical techniques to derive the impulse response. One common approach is polynomial division. In this method, the input and output sequences are treated as coefficients of...
Deconvolution involves several mathematical techniques to derive the impulse response. One common approach is polynomial division. In this method, the input and output sequences are treated as coefficients of...
Definition of z-Transform
The z-transform is a powerful mathematical tool used in the analysis of discrete-time signals and systems. It is an essential analytical tool, analogous to the Laplace transform used in continuous-time systems. It plays a crucial role in the analysis of signals and systems, complementing the discrete-time Fourier transform. Both the z-transform and the Laplace transform convert differential or difference equations into algebraic equations, simplifying the process of solving complex problems.
Properties of the z-Transform I
The z-transform is a fundamental tool in digital signal processing, enabling the analysis of discrete-time systems through its various properties. It is an invaluable tool for analyzing discrete-time systems, offering a range of properties that simplify complex signal manipulations. One fundamental property is linearity. For any two discrete-time signals, the z-transform of their linear combination equals the same linear combination of their individual z-transforms. This property is essential...
Inverse z-Transform by Partial Fraction Expansion
The inverse z-transform is a crucial technique for converting a function from its z-domain representation back to the time domain. One effective method for finding the inverse z-transform is the Partial Fraction Method, which involves decomposing a function into simpler fractions with distinct coefficients. These fractions correspond to known z-transform pairs, facilitating the inverse transformation process.
To begin the process, the poles of the function are identified and the function is...
To begin the process, the poles of the function are identified and the function is...
Transformations of Functions III
Transformations modify the graphical representation of a function without changing its fundamental form. One common transformation is reflection, which flips the graph across a designated axis. When the vertical coordinates of all points are multiplied by the negative one, the entire graph is mirrored over the horizontal axis. This transformation reverses the vertical orientation of peaks and troughs, akin to signal inversion in electrical systems, where a waveform is flipped, but the timing of...


