用张量分解压缩模型参数,提升三维地震反演的精度与稳定性。
Tensor Train Decomposition-based 3D Implicit Full Waveform Inversion with Multi-scale Structural Similarity

- 用张量列车分解重参数化速度模型,降低内存消耗。
- 多尺度结构相似性目标函数缓解周期跳跃问题。
- 适合初值差或缺少低频数据的复杂地质反演任务。
三维全波形反演(3DFWI)是重建高分辨率地下速度模型的强大技术,但受限于高内存需求、计算成本及对周期跳跃的敏感性。为此,我们提出基于张量列车(TT)分解的三维隐式全波形反演框架(TT-3DIFWI),结合多尺度结构相似性(M-SSIM)目标函数。该框架将三维速度模型表示为一系列低秩核心张量的乘积,通过三个轴向独立的隐式神经网络表示(INR)以一维坐标为输入预测这些核心张量,而非直接预测速度场。该方法显著降低INR训练内存开销,同时保持重建精度与分辨率。此外,TT的低秩结构保障了重建结果的结构一致性,提升反演精度与连续性。M-SSIM目标函数可比较预测与观测数据在多尺度下的结构差异,并利用超低频特征缓解周期跳跃问题。合成与复杂陆上数据集的数值实验表明,即使初始模型不佳或缺失低频信息,TT-3DIFWI仍能实现准确、连续的速度重建。
原文摘要 · Abstract (English)
Three-dimensional full waveform inversion (3DFWI) is a powerful technique for reconstructing high-resolution subsurface velocity models. However, its application is often limited by high memory requirements, computational costs, and sensitivity to cycle skipping. To overcome these challenges, we propose a novel tensor train (TT) decomposition-based 3D implicit full waveform inversion framework (TT-3DIFWI) combined with a multi-scale structural similarity (M-SSIM) objective function. In this framework, the 3D velocity model is represented by TT decomposition as a product of a series of low-rank core tensors. Then, three axis-specific implicit neural network representations (INR) based on one-dimensional vector coordinates as input are constructed to predict these core tensors, rather than directly predicting the velocity model. This INR reparameterization method based on TT decomposition can significantly reduce the memory consumption of INR training while maintaining the accuracy and resolution of the 3D velocity model reconstruction. Meanwhile, the low-rank structure of TT decomposition also ensures the structural consistency of the reconstruction velocity, thereby improving the accuracy and continuity of the inversion result. Furthermore, the M-SSIM objective function can compare the multi-scale structural differences between predicted and observed data, and utilize the ultra-low frequency features to reduce cycle skipping. Numerical experiments on synthetic and challenging land datasets demonstrate that TT-3DIFWI with M-SSIM achieves accurate and continuous velocity reconstruction, even with poor initial models or missing low-frequency data.
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