基于合成数据训练的U-net的剪切波和深度学习的近地表速度估计

Taneesh Gupta , Paul Zwartjes , Udbhav Bamba , Koustav Ghosal , Deepak K. Gupta
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引用次数: 0

摘要

在复杂的近地表条件下估计良好的速度模型仍然是一个正在进行的研究课题。我们建议使用深度神经网络以数据驱动的方式预测从表面波转换到相速度-频率面板的近地表速度剖面。这与最近许多试图从直接反射的体波或导波中估计速度的工作不同。第二个目标是分析各种常用的深度学习实践(如迁移学习和数据增强)对预测精度的影响。通过对合成数据和实际地球物理实例的数值实验,我们证明了迁移学习和数据增强在使用深度学习进行速度估计时是有用的。第三个也是最后一个目标是研究在我们的问题背景下,分布外(OOD)数据的深度学习模型缺乏泛化,并提出一种新的方法来解决它。我们提出了一个领域自适应网络,用于训练深度学习模型,该模型使用关于速度值范围的先验知识来约束输出的映射。对现场数据(不属于训练数据的一部分)的最后比较表明,深度神经网络预测结果优于利用频散曲线反演工作流获得的传统速度模型估计结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Near-surface velocity estimation using shear-waves and deep-learning with a U-net trained on synthetic data

Estimation of good velocity models under complex near-surface conditions remains a topic of ongoing research. We propose to predict near-surface velocity profiles from surface-waves transformed to phase velocity-frequency panels in a data-driven manner using deep neural networks. This is a different approach from many recent works that attempt to estimate velocity from directly reflected body waves or guided waves. A secondary objective is to analyze the influence on the prediction accuracy of various commonly employed deep learning practices, such as transfer learning and data augmentations. Through numerical experiments on synthetic data as well as a real geophysical example, we demonstrate that transfer learning as well as data augmentations are helpful when using deep learning for velocity estimation. A third and final objective is to study lack of generalization of deep learning models for out-of-distribution (OOD) data in the context of our problem, and present a novel approach to tackle it. We propose a domain adaptation network for training deep learning models that uses a priori knowledge on the range of velocity values in order to constrain mapping of the output. The final comparison on field data, which was not part of the training data, show the deep neural network predictions compare favorably with a conventional velocity model estimation obtained with a dispersion curve inversion workflow.

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