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dc.contributor.authorJones, Christopher D.
dc.contributor.authorJackson, Darrell R.
dc.date.accessioned2018-10-11T14:08:15Z
dc.date.available2018-10-11T14:08:15Z
dc.date.issued1997
dc.identifier11477
dc.identifier.govdocCP-45
dc.identifier.urihttp://hdl.handle.net/20.500.12489/432
dc.description.abstractBiological activity in marine sediments creates a time-varying, randomly fluctuating medium. A bio-diffusive model is proposed for predicting the temporal and spatial spectrum of sediment density fluctuations. Perturbation theory is used to model sediment volume scattering and the temporal correlation of the scattered field. These models are compared with field data recorded in a biologically active shallow water environment, and sediment blo-diffusion parameters are estimated.
dc.format8 p. : ill. ; digital, PDF file
dc.languageEnglish
dc.publisherNATO. SACLANTCEN
dc.sourceIn: High Frequency Seafloor Acoustics (SACLANTCEN Conference Proceedings CP-45), 1997, pp. 275-282
dc.subjectAcoustic scattering - Seafloor and sea surface
dc.subjectAcoustic scattering - Biologic
dc.subjectSeafloor sediments
dc.subjectPerturbation (Mathematics)
dc.subjectAcoustic models
dc.titleTemporal fluctuation of backscattered field due to bioturbatioon in marine sediments
dc.typePapers and Articles
dc.typeConference Proceedings (CP)


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