In:
The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 119, No. 5_Supplement ( 2006-05-01), p. 3253-3253
Abstract:
The upper medium is sea water, and the bottom medium is a marine sediment whose physical description is consistent with the theory advanced by Frenkel in 1944 and with the model proposed by Biot in 1961 for a porous medium at low frequencies. Within the sediment, three generic types (modes) of wavelike disturbances are possible. These three modes are here termed the acoustic, shear, and Darcy modes. The first two are governed by propagating wave equations and the third by a diffusion equation. The first and third are dilatational. All three are nominally uncoupled, although coupling occurs at interfaces. When an obliquely incident acoustic wave impinges from the water on the interface, all three types of disturbances are in principle excited in the sediment, and the details of the excitation are governed by interface conditions, whose derivation is reported in the present paper. Each mode has its own characteristic parameters, and the sediment reflection coefficient, considered as a function of angle of incidence and of frequency, implicitly depends on all of these parameters. The question is addressed as to how, given such reflection coefficient data, one might extract the parameters for the Darcy mode for representative realistic experimental circumstances.
Type of Medium:
Online Resource
ISSN:
0001-4966
,
1520-8524
Language:
English
Publisher:
Acoustical Society of America (ASA)
Publication Date:
2006
detail.hit.zdb_id:
1461063-2
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