Simultaneous P- and S-wave seismic traveltime tomography using physics-informed neural networks

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Chao Song, Hang Geng, Yufeng Wang, Umair Bin Waheed, Cai Liu
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引用次数: 0

Abstract

Seismic tomography has long been an effective tool for constructing reliable subsurface structures. However, simultaneous inversion of P- and S-wave velocities presents a significant challenge for conventional seismic tomography methods, which depend on numerical algorithms to calculate traveltimes. A physics-informed neural network—based seismic tomography method (PINNtomo) has been proposed to solve the eikonal equation and construct the velocity model. We propose extending PINNtomo to perform multiparameter inversion of P- and S-wave velocities jointly, which we refer to as PINNPStomo. In PINNPStomo, we employ two neural networks: one for the P- and S-wave traveltimes and another for the P- and S-wave velocities. By optimizing the misfits of P- and S-wave first-arrival traveltimes calculated from the eikonal equations, we can obtain the predicted P- and S-wave velocities that determine these traveltimes. Recognizing that the original PINNtomo utilizes a multiplicative factored eikonal equation, which depends on background traveltimes corresponding to a homogeneous velocity at the source location, we propose to use an effective-slowness-based factored eikonal equation for PINNPStomo to eliminate this dependency. The proposed PINNPStomo, incorporating the effective-slowness-based factored eikonal equation, demonstrates superior convergence speed and multiparameter inversion accuracy. We validate these improvements using two-dimensional Marmousi, two-dimensional Overthrust and three-dimensional foothill elastic velocity models across three different seismic data acquisition geometries.

同时使用物理信息神经网络的P波和s波地震走时层析成像
地震层析成像一直是构建可靠地下结构的有效工具。然而,纵波和横波速度的同时反演对传统的地震层析成像方法提出了重大挑战,这些方法依赖于数值算法来计算传播时间。提出了一种基于物理信息神经网络的地震层析成像方法(PINNtomo),用于求解斜向方程和构建速度模型。我们提出对PINNtomo进行扩展,使其能够同时进行横波速度和纵波速度的多参数反演,我们称之为PINNPStomo。在PINNPStomo中,我们使用了两个神经网络:一个用于P波和s波传播时间,另一个用于P波和s波速度。通过优化由方程计算的横波和纵波初到行时的失配,我们可以得到决定这些行时的预测横波速度。认识到原始的PINNtomo使用乘法因子方程,该方程依赖于对应于源位置均匀速度的背景旅行时间,我们建议使用基于有效慢度的因子方程来消除这种依赖性。该方法结合了基于有效慢度的因子方程,具有较好的收敛速度和多参数反演精度。我们通过三种不同的地震数据采集几何形状,使用二维Marmousi、二维逆冲断层和三维山麓弹性速度模型验证了这些改进。
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
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