Abstract
The diffusive-viscous wave equation arises in a variety of applications in geophysics such as the attenuation of seismic waves propagating in fluid-saturated solids, and frequency-dependent phenomena in porous media. This paper provides a well-posedness analysis on the initial-boundary value problem of the diffusive-viscous wave equation.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
