Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

The waveform comparison of three common-used fractional viscous acoustic wave equations

View through CrossRef
Abstract The forward simulation of the viscous acoustic wave equation is an essential part of geophysics and energy resources exploration research. The viscous acoustic seismic wave equations are diverse, even if we limit the study scope to the fractional viscous wave equations. In the present study, we consider three commonly used fractional-order viscous wave equations: the fractional viscous acoustic wave (FVAW) equation, dispersion-dominated wave (DDW) equation, and attenuation-dominated wave (ADW) equation. The acoustic wave (AW) equation, as a special fractional wave equation, is used to compare with the three viscous acoustic equations. The asymptotic local finite difference (ALFD) method is adopted to solve the three fractional wave equations, while the Lax-Wendroff Correction (LWC) scheme is used to solve the integer wave equation. The analysis shows that the stability of the ADW equation is the most rigorous, and that of the DDW equation is the most flexible. When the numerical wave number \(\vartheta =\pi\), the maximum phase velocity errors of the FVAW equation, DDW equation, ADW equation, and AW equation are 27.78%, 28.02%, 2.25%, and 3.04%, respectively. Numerical experiments show that the waveforms simulated by the four equations with the same parameters are distinct. Specifically, the FVAW equation, DDW equation, and quality factor Q are sensitive to the arrival time, while the FVAW equation, ADW equation, and quality factor Q are sensitive to the amplitude. Furthermore, the change of amplitude is more apparent than that of the arrival time, giving the results that the arrival time is more robust than the amplitude.
Title: The waveform comparison of three common-used fractional viscous acoustic wave equations
Description:
Abstract The forward simulation of the viscous acoustic wave equation is an essential part of geophysics and energy resources exploration research.
The viscous acoustic seismic wave equations are diverse, even if we limit the study scope to the fractional viscous wave equations.
In the present study, we consider three commonly used fractional-order viscous wave equations: the fractional viscous acoustic wave (FVAW) equation, dispersion-dominated wave (DDW) equation, and attenuation-dominated wave (ADW) equation.
The acoustic wave (AW) equation, as a special fractional wave equation, is used to compare with the three viscous acoustic equations.
The asymptotic local finite difference (ALFD) method is adopted to solve the three fractional wave equations, while the Lax-Wendroff Correction (LWC) scheme is used to solve the integer wave equation.
The analysis shows that the stability of the ADW equation is the most rigorous, and that of the DDW equation is the most flexible.
When the numerical wave number \(\vartheta =\pi\), the maximum phase velocity errors of the FVAW equation, DDW equation, ADW equation, and AW equation are 27.
78%, 28.
02%, 2.
25%, and 3.
04%, respectively.
Numerical experiments show that the waveforms simulated by the four equations with the same parameters are distinct.
Specifically, the FVAW equation, DDW equation, and quality factor Q are sensitive to the arrival time, while the FVAW equation, ADW equation, and quality factor Q are sensitive to the amplitude.
Furthermore, the change of amplitude is more apparent than that of the arrival time, giving the results that the arrival time is more robust than the amplitude.

Related Results

Solving Undamped and Damped Fractional Oscillators via Integral Rohit Transform
Solving Undamped and Damped Fractional Oscillators via Integral Rohit Transform
Background: The dynamics of fractional oscillators are generally described by fractional differential equations, which include the fractional derivative of the Caputo or Riemann-Li...
Soham Transform in Fractional Differential Equations
Soham Transform in Fractional Differential Equations
Objectives: Soham transforms is one of the appropriate tools for solving fractional differential equations that are flexible enough to adapt to different purposes. Methods: Integra...
Sea Surface Height Estimation from Improved Modified, and Decontaminated Sub-Waveform Retracking Methods over Coastal Areas
Sea Surface Height Estimation from Improved Modified, and Decontaminated Sub-Waveform Retracking Methods over Coastal Areas
Coastal zones are challenging areas for sensing by satellite altimeters because reflected signals from non-water surfaces and from calm sea surfaces in small bays and ports inside ...
Wave Force Calculations for Stokes and Non-Stokes Waves
Wave Force Calculations for Stokes and Non-Stokes Waves
ABSTRACT A new wave particle velocity procedure permits calculation of forces from regular wave profiles of more or less arbitrary wave crest to height ratios, as...
Hurricane Eloise Directional Wave Energy Spectra
Hurricane Eloise Directional Wave Energy Spectra
ABSTRACT Directiona1 wave energy spectra, calculated from data recorded during Hurricane Eloise (Gulf of Mexico, 1975), are presented. The spectra, based on an en...
Gohar Fractional Derivative: Theory and Applications
Gohar Fractional Derivative: Theory and Applications
The local fractional derivatives marked the beginning of a new era in fractional calculus. Due to their that have never been observed before in the field, they are able to fill in ...
Receiver Balancing In Off-Centered Acoustic Logging Data
Receiver Balancing In Off-Centered Acoustic Logging Data
Abstract Modern multi-pole acoustic logging tools require addition and subtraction of signals from different combinations of receivers. To enable the correct subt...
RELATIONSHIP BETWEEN ATRIAL FIBRILLATION CARDIOVERSION AND F
RELATIONSHIP BETWEEN ATRIAL FIBRILLATION CARDIOVERSION AND F
Objectives To investigate the relationship between atrial fibrillation cardioversion and f wave in electrocardiogram, providing an ordinary and noninvasive method...

Back to Top