The transient and impulse responses (Green's function) for one-dimensional wave propagation in a standard linear solid are calculated using a Laplace Transform method. The spectrum of relaxation times is chosen so as to model a constant Q medium within an absorption band covering a broad frequency range which may be chosen so as to include the seismic frequencies. The inverse transform may be evaluated asymptotically in the limit of very long propagation times using the saddle point method. For shorter propagation times the method of steepest descent may be modified so as to yield an accurate first motion approximation. The character of the small amplitude precursor to the large amplitude ‘visible’ signal is investigated analytically. It is...
The transient response of one-dimensional nonuniform dispersive media is studied through the use of ...
Wave motion lies at the heart of many disciplines in the physical sciences and engineering. For exam...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
The transient and impulse responses (Green's function) for one-dimensional wave propagation in a sta...
We investigate one-dimensional waves in a standard linear solid for geophysically relevant ranges of...
A linear model for attenuation of waves is presented, with Q, or the portion of energy lost during e...
The propagation of plane waves through statistically layered media is investigated both numerically ...
I present a new time-domain method for solving for the stress and particle velocity of normally inci...
As a dynamic response, the wave propagation phenomenon usually varies with different media. In this ...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
The concept of a relaxation spectrum is used to compute the absorption and dispersion of a linear an...
The influence of attenuation on pulsed ultrasonic signals has been under intense investigation espec...
Because of the presence of structural defects such as microcracks and grain boundaries, the effectiv...
As seismic waves travel through the earth, the visco-elasticity of the earth's medium will cause ene...
A 1-D model is presented that couples the microscale oscillations of non-wetting fluid blobs in a pa...
The transient response of one-dimensional nonuniform dispersive media is studied through the use of ...
Wave motion lies at the heart of many disciplines in the physical sciences and engineering. For exam...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
The transient and impulse responses (Green's function) for one-dimensional wave propagation in a sta...
We investigate one-dimensional waves in a standard linear solid for geophysically relevant ranges of...
A linear model for attenuation of waves is presented, with Q, or the portion of energy lost during e...
The propagation of plane waves through statistically layered media is investigated both numerically ...
I present a new time-domain method for solving for the stress and particle velocity of normally inci...
As a dynamic response, the wave propagation phenomenon usually varies with different media. In this ...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
The concept of a relaxation spectrum is used to compute the absorption and dispersion of a linear an...
The influence of attenuation on pulsed ultrasonic signals has been under intense investigation espec...
Because of the presence of structural defects such as microcracks and grain boundaries, the effectiv...
As seismic waves travel through the earth, the visco-elasticity of the earth's medium will cause ene...
A 1-D model is presented that couples the microscale oscillations of non-wetting fluid blobs in a pa...
The transient response of one-dimensional nonuniform dispersive media is studied through the use of ...
Wave motion lies at the heart of many disciplines in the physical sciences and engineering. For exam...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...