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Influence of depth-dependent sedimen...

Joussein, Marianne.

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Influence of depth-dependent sediment properties on the pressure reflection coefficient at normal incidence using the Biot-Stoll model.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Influence of depth-dependent sediment properties on the pressure reflection coefficient at normal incidence using the Biot-Stoll model./
作者:	Joussein, Marianne.
面頁冊數:	107 p.
附註:	Source: Masters Abstracts International, Volume: 43-01, page: 0296.
Contained By:	Masters Abstracts International43-01.
標題:	Engineering, Marine and Ocean. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1421710
ISBN:	0496264559

Influence of depth-dependent sediment properties on the pressure reflection coefficient at normal incidence using the Biot-Stoll model.
Joussein, Marianne.

Influence of depth-dependent sediment properties on the pressure reflection coefficient at normal incidence using the Biot-Stoll model. - 107 p.

Source: Masters Abstracts International, Volume: 43-01, page: 0296.

Thesis (M.S.)--Florida Atlantic University, 2004.

The impact of depth-dependent geophysical parameters on the acoustic pressure reflection coefficient is studied at normal incidence using the Biot-Stoll theory in porous marine sediments. The seabed is modeled as a sediment layer with depth-dependent properties on top of a homogeneous half-space, as originally proposed by Stern. There is no discontinuity in sediment properties between the layer and the half-space. The reflection coefficient is determined by the evaluation of boundary conditions at the water-sediment layer interface and the sediment layer-half-space interface. Results are obtained for different types of sediment, from medium size sands to silty clay, and different porosity profiles vs. depth.

ISBN: 0496264559Subjects--Topical Terms:

1019064
Engineering, Marine and Ocean.

Influence of depth-dependent sediment properties on the pressure reflection coefficient at normal incidence using the Biot-Stoll model.
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500 $a Adviser: Pierre-Philippe J. Beaujean.
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520 $a The impact of depth-dependent geophysical parameters on the acoustic pressure reflection coefficient is studied at normal incidence using the Biot-Stoll theory in porous marine sediments. The seabed is modeled as a sediment layer with depth-dependent properties on top of a homogeneous half-space, as originally proposed by Stern. There is no discontinuity in sediment properties between the layer and the half-space. The reflection coefficient is determined by the evaluation of boundary conditions at the water-sediment layer interface and the sediment layer-half-space interface. Results are obtained for different types of sediment, from medium size sands to silty clay, and different porosity profiles vs. depth.
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