一种衰减及速度各向异性介质地震波数值模拟方法及系统

By constructing a pure pseudo-longitudinal wave fractional-order Laplace operator viscous acoustic wave equation for attenuation and velocity anisotropic media, the problem that existing technologies cannot accurately describe attenuation and velocity anisotropy effects is solved, and accurate quantitative simulation of seismic wave propagation characteristics in strongly attenuated and anisotropic media is realized.

CN117094147BActive Publication Date: 2026-07-17CHINA UNIV OF PETROLEUM (EAST CHINA)

Patent Information

Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
CHINA UNIV OF PETROLEUM (EAST CHINA)
Filing Date
2023-08-18
Publication Date
2026-07-17

AI Technical Summary

Technical Problem

Existing wave equations cannot accurately characterize the attenuation anisotropy and velocity anisotropy effects of pure wave modes, especially in strongly attenuated and velocity-anisotropic media, making it difficult to achieve an accurate quantitative description of seismic wave propagation characteristics.

Method used

A pseudo-longitudinal wave equation with fractional-order Laplace operator for attenuated and velocity-anisotropic media containing a single component is constructed. Combined with the generalized viscoelastic anisotropic constitutive relation and the anisotropic constant quality factor model, the seismic wave field is solved by the pseudospectral method, and the seismic wave equation for attenuated and velocity-anisotropic media is established.

Benefits of technology

It can accurately describe the attenuation and velocity anisotropy effects of seismic waves in strongly attenuated and anisotropic media, effectively describe the decoupled amplitude attenuation and phase delay characteristics, and improve the accuracy of numerical simulation of seismic waves.

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Abstract

本发明公开一种衰减及速度各向异性介质地震波数值模拟方法及系统,涉及地震勘探领域,该方法包括:根据地质地球物理任务,构建目标地区地震地球物理模型并确定地震子波类型及地震子波主频;根据目标地区地震地球物理模型以及预设的地震子波类型和地震子波主频,构建衰减及速度各向异性介质地震波动方程;根据衰减及速度各向异性介质地震波动方程的稳定性条件,确定数值模拟的时间步长;根据数值模拟的时间步长、目标地区地震地球物理模型、地震子波类型及地震子波主频,利用伪谱法,对衰减及速度各向异性介质地震波动方程进行求解,得到地震波场。本发明能够提高强衰减及各向异性介质中地震波传播特征的准确性。
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