A one-dimensional, randomly stratified model of ocean sediments

The reflection of a monochromatic acoustic plane wave from ocean sedimentary layers is considered in the context of a one-dimensional refractive, randomly stratified and dissipative multilayer model. Simulations and analysis are used to study the structure of the fields within the sediments, as well...

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Veröffentlicht in:Wave motion 1988, Vol.10 (5), p.421-441
1. Verfasser: Kohler, Werner E.
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container_title Wave motion
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creator Kohler, Werner E.
description The reflection of a monochromatic acoustic plane wave from ocean sedimentary layers is considered in the context of a one-dimensional refractive, randomly stratified and dissipative multilayer model. Simulations and analysis are used to study the structure of the fields within the sediments, as well as the interface reflection properties, over a wide range of frequencies and incidence angles. Some insights into the experimentally observed phenomenon of negative bottom loss frequency dependence are obtained.
doi_str_mv 10.1016/0165-2125(88)90046-7
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subjects Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
Marine geology
title A one-dimensional, randomly stratified model of ocean sediments
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