用物理约束的生成对抗网络改进地震反演,提升复杂地质下的成像稳定性。
Seismic full-waveform inversion based on a physics-driven generative adversarial network
- 结合地震波方程物理约束与生成对抗网络,增强反演鲁棒性。
- 在两个基准模型上实现更高结构相似性(SSIM)和信噪比(SNR)。
- 适合需要高精度地下速度建模的地震勘探与资源探测领域。
全波形反演(FWI)是一种高分辨率地球物理成像技术,通过迭代最小化预测与观测地震数据之间的偏差来重建地下速度模型。然而,在复杂地质条件下,传统FWI严重依赖初始模型,且在数据稀疏或含噪声时易产生不稳定结果。本文提出一种基于物理驱动的生成对抗网络全波形反演方法,将深度神经网络的数据驱动能力与地震波方程的物理约束相结合,并通过判别器进行对抗训练,以提升反演结果的稳定性与鲁棒性。在两个代表性基准地质模型上的实验表明,该方法能有效恢复复杂速度结构,在结构相似性(SSIM)和信噪比(SNR)方面均表现优异。该方法为缓解全波形反演对初始模型的依赖提供了有效方案,具有良好的实际应用前景。
原文摘要 · Abstract (English)
Objectives: Full-waveform inversion (FWI) is a high-resolution geophysical imaging technique that reconstructs subsurface velocity models by iteratively minimizing the misfit between predicted and observed seismic data. However, under complex geological conditions, conventional FWI suffers from strong dependence on the initial model and tends to produce unstable results when the data are sparse or contaminated by noise. Methods: To address these limitations, this paper proposes a physics-driven generative adversarial network-based full-waveform inversion method. The proposed approach integrates the data-driven capability of deep neural networks with the physical constraints imposed by the seismic wave equation, and employs adversarial training through a discriminator to enhance the stability and robustness of the inversion results. Results: Experimental results on two representative benchmark geological models demonstrate that the proposed method can effectively recover complex velocity structures and achieves superior performance in terms of structural similarity (SSIM) and signal-to-noise ratio (SNR). Conclusions: This method provides a promising solution for alleviating the initial-model dependence in full-waveform inversion and shows strong potential for practical applications.
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