The influence of finely layered seabeds on acoustic propagation in shallow water

Except in the deep ocean, the seabed has a major influence on low-frequency acoustic propagation. The formulation of an adequate geoacoustic model of the seabed is therefore one of the most important tasks facing anyone carrying out acoustic propagation modelling to predict underwater sound levels i...

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Main Authors: Duncan, Alec, Gavrilov, Alexander, Koessler, Matthew Walter
Other Authors: Mr Terry McMinn
Format: Conference Paper
Published: Australian Acoustical Society 2014
Online Access:http://www.acoustics.asn.au/conference_proceedings/INTERNOISE2014/papers/p700.pdf
http://hdl.handle.net/20.500.11937/40156
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author Duncan, Alec
Gavrilov, Alexander
Koessler, Matthew Walter
author2 Mr Terry McMinn
author_facet Mr Terry McMinn
Duncan, Alec
Gavrilov, Alexander
Koessler, Matthew Walter
author_sort Duncan, Alec
building Curtin Institutional Repository
collection Online Access
description Except in the deep ocean, the seabed has a major influence on low-frequency acoustic propagation. The formulation of an adequate geoacoustic model of the seabed is therefore one of the most important tasks facing anyone carrying out acoustic propagation modelling to predict underwater sound levels in coastal and continental shelf waters. It is often assumed that seabed layering on scales significantly smaller than the acoustic wavelength can be ignored when carrying out such modelling, and that these layers can instead be replaced by a simplified model involving a small number of layers in which the geoacoustic parameters vary smoothly with depth. This paper explores this assumption, with particular reference to the finely layered elastic seabeds typical of the Australian continental shelf. This investigation is based on a comparison of the plane-wave reflection coefficient vs grazing angle curves of these two representations of the seabed.
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spelling curtin-20.500.11937-401562017-01-30T14:40:10Z The influence of finely layered seabeds on acoustic propagation in shallow water Duncan, Alec Gavrilov, Alexander Koessler, Matthew Walter Mr Terry McMinn Except in the deep ocean, the seabed has a major influence on low-frequency acoustic propagation. The formulation of an adequate geoacoustic model of the seabed is therefore one of the most important tasks facing anyone carrying out acoustic propagation modelling to predict underwater sound levels in coastal and continental shelf waters. It is often assumed that seabed layering on scales significantly smaller than the acoustic wavelength can be ignored when carrying out such modelling, and that these layers can instead be replaced by a simplified model involving a small number of layers in which the geoacoustic parameters vary smoothly with depth. This paper explores this assumption, with particular reference to the finely layered elastic seabeds typical of the Australian continental shelf. This investigation is based on a comparison of the plane-wave reflection coefficient vs grazing angle curves of these two representations of the seabed. 2014 Conference Paper http://hdl.handle.net/20.500.11937/40156 http://www.acoustics.asn.au/conference_proceedings/INTERNOISE2014/papers/p700.pdf Australian Acoustical Society restricted
spellingShingle Duncan, Alec
Gavrilov, Alexander
Koessler, Matthew Walter
The influence of finely layered seabeds on acoustic propagation in shallow water
title The influence of finely layered seabeds on acoustic propagation in shallow water
title_full The influence of finely layered seabeds on acoustic propagation in shallow water
title_fullStr The influence of finely layered seabeds on acoustic propagation in shallow water
title_full_unstemmed The influence of finely layered seabeds on acoustic propagation in shallow water
title_short The influence of finely layered seabeds on acoustic propagation in shallow water
title_sort influence of finely layered seabeds on acoustic propagation in shallow water
url http://www.acoustics.asn.au/conference_proceedings/INTERNOISE2014/papers/p700.pdf
http://hdl.handle.net/20.500.11937/40156