Green' function representation for acoustic pressure over a poroelastic seabedFootnote^∗

^∗This research was supported in part by the National Science Foundation through grant BES-9402539.

References

• Beebe , J.H. , McDaniel , S.T. and Rubano , L.A. 1982 . Shallow-water transmission loss prediction using the biot sediment model . J. Acoust. Soc. Am , 71 ( 6 ) : 1417 – 1426 .
   Web of Science ®Google Scholar
• Biot , M.A. 1956 . Theory of propogation of elastic waves in a fluid-saturated porous solid.i. lower frequency range . J. Acoust. Soc. Am , 28 ( 2 ) : 168 – 178 .
   Web of Science ®Google Scholar
• Biot , M.A. 1956 . Theory of propogation of elastic waves in a fluid-saturated porous solid.ii. higher frequency range . J. Acoust. Soc. Am , 28 ( 2 ) : 179 – 191 .
   Web of Science ®Google Scholar
• Buchanan J.L. Gilbert R.P. Transmussion loss in the far field over aone-layer seaded assuming the biot sediment model ZAMM. To appear
   Google Scholar
• Buchanan , J.L. and Gilbert , R.p. 1996 . Transmission loss in the far field over a seabed with rigid substrate assuming the biot sediment model . Journal of Computational Acoustics , 4 ( 1 ) : 29 – 54 .
   Web of Science ®Google Scholar
• Buchanan J.L. Gilbert R.P. Comparison of the solution to a problem in ocean acoustics by parabolic approximatin with the exact solution obtained from the residue calculus. In Proceedings of the Conference on Generalized Analytic Functions Graz Austria 1997 Submitted
   Google Scholar
• Holland , C.W. and Brounson , B.A. 1437 . The biot-stoll sediment model: An experimental assessment . J. Acoust. Soc. Am , 84 ( 4 ) : 1443 – 1988 .
   Google Scholar