arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2007.08330physics.comp-phmath-phmath.MP
收藏

PINNeik:使用物理信息神经网络的Eikonal解决方案

PINNeik: Eikonal solution using physics-informed neural networks

Umair bin Waheed, Ehsan Haghighat, Tariq Alkhalifah, Chao Song, Qi Hao

摘要:

程函方程在科学和工程学科中广泛使用。在地震学中,它调节震源定位、成像和反演等应用所需的地震波走时。多年来,已经开发了几种数值算法来求解程函方程。然而,这些方法需要相当大的修改,以纳入额外的物理,如各向异性,甚至可能分解为某些复杂形式的程函方程,需要近似方法。此外,当对于速度模型和/或源位置中的扰动需要重复计算时,特别是在大型3D模型中,它们遭受计算瓶颈。在这里,我们提出了一个算法来解决程函方程的基础上新兴的范式的物理信息神经网络(PINNs)。通过最小化由施加程函方程形成的损失函数,我们训练神经网络输出与基本偏微分方程一致的旅行时。我们观察到足够高的走时精度为大多数感兴趣的应用程序。我们还演示了所提出的算法如何利用机器学习技术,如转移学习和代理建模,以加快旅行时计算更新的速度模型和源位置。此外,我们使用一个局部自适应激活函数和自适应加权的损失函数中的条款,以提高收敛速度和解决方案的精度。我们还显示了该方法的灵活性,将介质各向异性和自由表面形貌相比,传统的方法,需要显着的算法修改。所提出的PINN程函求解器的这些属性对于获得地震应用的灵活且高效的正演建模引擎来说是非常理想的。

英文摘要:

The eikonal equation is utilized across a wide spectrum of science and engineering disciplines. In seismology, it regulates seismic wave traveltimes needed for applications like source localization, imaging, and inversion. Several numerical algorithms have been developed over the years to solve the eikonal equation. However, these methods require considerable modifications to incorporate additional physics, such as anisotropy, and may even breakdown for certain complex forms of the eikonal equation, requiring approximation methods. Moreover, they suffer from computational bottleneck when repeated computations are needed for perturbations in the velocity model and/or the source location, particularly in large 3D models. Here, we propose an algorithm to solve the eikonal equation based on the emerging paradigm of physics-informed neural networks (PINNs). By minimizing a loss function formed by imposing the eikonal equation, we train a neural network to output traveltimes that are consistent with the underlying partial differential equation. We observe sufficiently high traveltime accuracy for most applications of interest. We also demonstrate how the proposed algorithm harnesses machine learning techniques like transfer learning and surrogate modeling to speed up traveltime computations for updated velocity models and source locations. Furthermore, we use a locally adaptive activation function and adaptive weighting of the terms in the loss function to improve convergence rate and solution accuracy. We also show the flexibility of the method in incorporating medium anisotropy and free-surface topography compared to conventional methods that require significant algorithmic modifications. These properties of the proposed PINN eikonal solver are highly desirable in obtaining a flexible and efficient forward modeling engine for seismological applications.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑