Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data

This paper focuses on acoustic reflectivity of the ocean bottom, and describes inversion of reflection data from an experiment designed to study the physical properties and structure of the ocean bottom. The formalism of Bayesian inference is reviewed briefly to establish an understanding of the app...

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Main Author: N. Ross Chapman
Format: Article
Language:English
Published: MDPI AG 2016-09-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:http://www.mdpi.com/2077-1312/4/3/61
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author N. Ross Chapman
author_facet N. Ross Chapman
author_sort N. Ross Chapman
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description This paper focuses on acoustic reflectivity of the ocean bottom, and describes inversion of reflection data from an experiment designed to study the physical properties and structure of the ocean bottom. The formalism of Bayesian inference is reviewed briefly to establish an understanding of the approach for inversion that is in widespread use. A Bayesian inversion of ocean bottom reflection coefficient versus angle data to estimate geoacoustic model parameters of young oceanic crust is presented. The data were obtained in an experiment to study the variation of sound speed in crustal basalt with age of the crust at deep water sites in the Pacific Ocean where the sediment deposits overlying the basalt are very thin. The inversion results show that sound speed of both compressional and shear waves is increasing with crustal age over the track of the experiment where age increased from 40 to 70 million years.
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spelling doaj.art-32472307f5684798a3f637b7951bf2902022-12-21T19:58:00ZengMDPI AGJournal of Marine Science and Engineering2077-13122016-09-01436110.3390/jmse4030061jmse4030061Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity DataN. Ross Chapman0School of Earth and Ocean Sciences, University of Victoria, Victoria, BC V8P5A4, CanadaThis paper focuses on acoustic reflectivity of the ocean bottom, and describes inversion of reflection data from an experiment designed to study the physical properties and structure of the ocean bottom. The formalism of Bayesian inference is reviewed briefly to establish an understanding of the approach for inversion that is in widespread use. A Bayesian inversion of ocean bottom reflection coefficient versus angle data to estimate geoacoustic model parameters of young oceanic crust is presented. The data were obtained in an experiment to study the variation of sound speed in crustal basalt with age of the crust at deep water sites in the Pacific Ocean where the sediment deposits overlying the basalt are very thin. The inversion results show that sound speed of both compressional and shear waves is increasing with crustal age over the track of the experiment where age increased from 40 to 70 million years.http://www.mdpi.com/2077-1312/4/3/61geoacoustic modelBayesian inferenceocean bottom reflection coefficientupper oceanic crustdeep water acousticsthin sediment
spellingShingle N. Ross Chapman
Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
Journal of Marine Science and Engineering
geoacoustic model
Bayesian inference
ocean bottom reflection coefficient
upper oceanic crust
deep water acoustics
thin sediment
title Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
title_full Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
title_fullStr Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
title_full_unstemmed Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
title_short Perspectives on Geoacoustic Inversion of Ocean Bottom Reflectivity Data
title_sort perspectives on geoacoustic inversion of ocean bottom reflectivity data
topic geoacoustic model
Bayesian inference
ocean bottom reflection coefficient
upper oceanic crust
deep water acoustics
thin sediment
url http://www.mdpi.com/2077-1312/4/3/61
work_keys_str_mv AT nrosschapman perspectivesongeoacousticinversionofoceanbottomreflectivitydata