Wave propagation in periodic fluid-solid layered media

Dispersion equation is derived for the Floquet waves in a horizontal periodically layered fluid-solid medium. It is shown that the dispersion equation consists of four factors. This representation explains the splitting of parameters (frequency, horizontal slowness) in passing and stop bands. The Fl...

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Date:2016
Main Authors: Roganov, Yu.V., Roganov, V.Yu.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016
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Online Access:https://journals.uran.ua/geofizicheskiy/article/view/91877
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Roganov, Yu.V.
Roganov, V.Yu.
author_facet Roganov, Yu.V.
Roganov, V.Yu.
author_sort Roganov, Yu.V.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:18:21Z
description Dispersion equation is derived for the Floquet waves in a horizontal periodically layered fluid-solid medium. It is shown that the dispersion equation consists of four factors. This representation explains the splitting of parameters (frequency, horizontal slowness) in passing and stop bands. The Floquet waves with horizontal group velocity can be computed individually from each of these factors. The properties of horizontally propagated waves are considered. The equations for the ratios of the components of polarization vectors and the amplitudes of partial waves are derived. Proposed theory is illustrated in one numerical example
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format Article
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institution Geofizicheskiy Zhurnal
language Russian
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publishDate 2016
publisher S. Subbotin Institute of Geophysics of the NAS of Ukraine
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spelling journalsuranua-geofizicheskiy-article-918772020-10-07T11:18:21Z Wave propagation in periodic fluid-solid layered media Roganov, Yu.V. Roganov, V.Yu. periodic fluid-solid medium dispersion equation Floquet wave slowness curve velocity indicatrix Dispersion equation is derived for the Floquet waves in a horizontal periodically layered fluid-solid medium. It is shown that the dispersion equation consists of four factors. This representation explains the splitting of parameters (frequency, horizontal slowness) in passing and stop bands. The Floquet waves with horizontal group velocity can be computed individually from each of these factors. The properties of horizontally propagated waves are considered. The equations for the ratios of the components of polarization vectors and the amplitudes of partial waves are derived. Proposed theory is illustrated in one numerical example S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/91877 10.24028/gzh.0203-3100.v38i6.2016.91877 Geofizicheskiy Zhurnal; Vol. 38 No. 6 (2016); 101-117 Геофизический журнал; Том 38 № 6 (2016); 101-117 Геофізичний журнал; Том 38 № 6 (2016); 101-117 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/91877/87650 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle periodic fluid-solid medium
dispersion equation
Floquet wave
slowness curve
velocity indicatrix
Roganov, Yu.V.
Roganov, V.Yu.
Wave propagation in periodic fluid-solid layered media
title Wave propagation in periodic fluid-solid layered media
title_full Wave propagation in periodic fluid-solid layered media
title_fullStr Wave propagation in periodic fluid-solid layered media
title_full_unstemmed Wave propagation in periodic fluid-solid layered media
title_short Wave propagation in periodic fluid-solid layered media
title_sort wave propagation in periodic fluid-solid layered media
topic periodic fluid-solid medium
dispersion equation
Floquet wave
slowness curve
velocity indicatrix
topic_facet periodic fluid-solid medium
dispersion equation
Floquet wave
slowness curve
velocity indicatrix
url https://journals.uran.ua/geofizicheskiy/article/view/91877
work_keys_str_mv AT roganovyuv wavepropagationinperiodicfluidsolidlayeredmedia
AT roganovvyu wavepropagationinperiodicfluidsolidlayeredmedia