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 |
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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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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.</description><identifier>ISSN: 0165-2125</identifier><identifier>EISSN: 1878-433X</identifier><identifier>DOI: 10.1016/0165-2125(88)90046-7</identifier><identifier>CODEN: WAMOD9</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Marine ; Marine geology</subject><ispartof>Wave motion, 1988, Vol.10 (5), p.421-441</ispartof><rights>1988</rights><rights>1989 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a387t-9fffb87c2c7702059e3ce14c9e9ee73f10906380ae246b7d15ed25bb489d774f3</citedby><cites>FETCH-LOGICAL-a387t-9fffb87c2c7702059e3ce14c9e9ee73f10906380ae246b7d15ed25bb489d774f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/0165212588900467$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,4010,27900,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=7234865$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Kohler, Werner E.</creatorcontrib><title>A one-dimensional, randomly stratified model of ocean sediments</title><title>Wave motion</title><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.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Marine</subject><subject>Marine geology</subject><issn>0165-2125</issn><issn>1878-433X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWKv_wMMeRBRcTTbJJrkopfgFBS8K3kI2mUBkd1OTrdB_77aVHj0Mc3ned5gHoXOCbwkm9d04vKxIxa-kvFYYs7oUB2hCpJAlo_TzEE32yDE6yfkLY0wEVRP0MCtiD6ULHfQ5xN60N0UyvYtduy7ykMwQfABXdNFBW0RfRAumLzJsE0M-RUfetBnO_vYUfTw9vs9fysXb8-t8tigNlWIolfe-kcJWVghcYa6AWiDMKlAAgnqCFa6pxAYqVjfCEQ6u4k3DpHJCME-n6HLXu0zxewV50F3IFtrW9BBXWRNOlBAcjyDbgTbFnBN4vUyhM2mtCdYbW3qjQm9UaCn11pYWY-zir99ka1o_OrAh77OiokzWfMTudxiMv_4ESDrbAL0ddSSwg3Yx_H_nF0jFfUw</recordid><startdate>1988</startdate><enddate>1988</enddate><creator>Kohler, Werner E.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>1988</creationdate><title>A one-dimensional, randomly stratified model of ocean sediments</title><author>Kohler, Werner E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a387t-9fffb87c2c7702059e3ce14c9e9ee73f10906380ae246b7d15ed25bb489d774f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Marine</topic><topic>Marine geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kohler, Werner E.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Wave motion</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kohler, Werner E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A one-dimensional, randomly stratified model of ocean sediments</atitle><jtitle>Wave motion</jtitle><date>1988</date><risdate>1988</risdate><volume>10</volume><issue>5</issue><spage>421</spage><epage>441</epage><pages>421-441</pages><issn>0165-2125</issn><eissn>1878-433X</eissn><coden>WAMOD9</coden><abstract>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. 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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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