In recent years, it has been recognized that the seismic wave equation solved with a finite-difference method in time causes a predictable and removable error through the use of so-called time-dispersion transforms. These transforms were thought not to apply to visco-elastic media. However, in this paper we demonstrate that the time-dispersion transforms remain applicable when the visco-elastic wave equation is solved with memory variables, as is commonly done. The crucial insight is that both the wave equation and the memory variables are computed with the same time-dispersion error. We show how the time-dispersion transforms can be implemented in, for example, MATLAB, and demonstrate the developed theory on a visco-elastic version of the ...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
Abstract. The diffusive-viscous wave equation plays an important role in seismic exploration and it ...
Real earth media disperse and attenuate propagating waves. This anelastic behavior can be well descr...
We derive an expression for the error introduced by the second-order accurate temporal finitediffere...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
Three numerical algorithms are proposed to solve the time-dependent elastodynamic equations in elast...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
Three numerical algorithms are proposed to solve the time-dependent elastodynamic equations in elast...
In this paper asymptotic dissipative waves in viscoanelastic media with shape and volumetric memory,...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
To model nonlinear viscous dissipative motions in solids, acoustical physicists usually add terms th...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
Abstract. The diffusive-viscous wave equation plays an important role in seismic exploration and it ...
Real earth media disperse and attenuate propagating waves. This anelastic behavior can be well descr...
We derive an expression for the error introduced by the second-order accurate temporal finitediffere...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
Three numerical algorithms are proposed to solve the time-dependent elastodynamic equations in elast...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
Three numerical algorithms are proposed to solve the time-dependent elastodynamic equations in elast...
In this paper asymptotic dissipative waves in viscoanelastic media with shape and volumetric memory,...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
To model nonlinear viscous dissipative motions in solids, acoustical physicists usually add terms th...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
Abstract. The diffusive-viscous wave equation plays an important role in seismic exploration and it ...
Real earth media disperse and attenuate propagating waves. This anelastic behavior can be well descr...