Abstract
A Green' function representation for acoustic pressure in an ocean over a poroelastic seabed is derived via a residue computation. Transmission loss curves for four sediments are computed using this representation and confirmed by comparison to the same curves computed by the numerical technique of parabolic approximation.
∗This research was supported in part by the National Science Foundation through grant BES-9402539.
†Supported in part by a US. Naval Academy Recognition Grant.
‡Supported in part by CECA Scholarship at the University of Tennessee at Chattanooga.
∗This research was supported in part by the National Science Foundation through grant BES-9402539.
†Supported in part by a US. Naval Academy Recognition Grant.
‡Supported in part by CECA Scholarship at the University of Tennessee at Chattanooga.
Notes
∗This research was supported in part by the National Science Foundation through grant BES-9402539.
†Supported in part by a US. Naval Academy Recognition Grant.
‡Supported in part by CECA Scholarship at the University of Tennessee at Chattanooga.