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Wavefield separation using a volume distribution of three component recordings
By making multiple three component (3C) measurements around a volume so that the rate of change of the wavefield in all directions can be estimated, it is possible to calculate the divergence and the curl of the wavefield which in turns corresponds to P‐ and S‐waves. The volume may be of arbitrary s...
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Published in: | Geophysical research letters 1999-09, Vol.26 (18), p.2821-2824 |
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container_title | Geophysical research letters |
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creator | Robertsson, Johan O. A. Muyzert, Everhard |
description | By making multiple three component (3C) measurements around a volume so that the rate of change of the wavefield in all directions can be estimated, it is possible to calculate the divergence and the curl of the wavefield which in turns corresponds to P‐ and S‐waves. The volume may be of arbitrary shape, but the equations for wavefield separation are simplified if the volume has a known shape such as that of a tetrahedron. The dimensions of the volume should be smaller than approximately one fifth of the minimum wavelength of the recorded wavefield.
A field test was carried out in Oman in April 1998. With a lack of distinct P‐ and S‐waves in the data, the technique was instead evaluated on the airwave‐induced ground motion. The airwave arrival was found to consist mainly of vertical motion that decays with depth. The wavefield separation technique was successfully tested on this arrival. |
doi_str_mv | 10.1029/1999GL010472 |
format | article |
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A field test was carried out in Oman in April 1998. With a lack of distinct P‐ and S‐waves in the data, the technique was instead evaluated on the airwave‐induced ground motion. The airwave arrival was found to consist mainly of vertical motion that decays with depth. The wavefield separation technique was successfully tested on this arrival.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/1999GL010472</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Arrivals ; Decay ; Earth sciences ; Earth, ocean, space ; Earthquakes, seismology ; Exact sciences and technology ; Field tests ; Ground motion ; Internal geophysics ; Mathematical analysis ; Recording ; Separation ; Wavelengths</subject><ispartof>Geophysical research letters, 1999-09, Vol.26 (18), p.2821-2824</ispartof><rights>Copyright 1999 by the American Geophysical Union.</rights><rights>1999 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4474-41f13b27bc4d11290d8fae1a6a663ed4c3d71f863b674c902a1e9e2a6723c6583</citedby><cites>FETCH-LOGICAL-c4474-41f13b27bc4d11290d8fae1a6a663ed4c3d71f863b674c902a1e9e2a6723c6583</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F1999GL010472$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F1999GL010472$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,11493,27901,27902,46443,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1943369$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Robertsson, Johan O. A.</creatorcontrib><creatorcontrib>Muyzert, Everhard</creatorcontrib><title>Wavefield separation using a volume distribution of three component recordings</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>By making multiple three component (3C) measurements around a volume so that the rate of change of the wavefield in all directions can be estimated, it is possible to calculate the divergence and the curl of the wavefield which in turns corresponds to P‐ and S‐waves. The volume may be of arbitrary shape, but the equations for wavefield separation are simplified if the volume has a known shape such as that of a tetrahedron. The dimensions of the volume should be smaller than approximately one fifth of the minimum wavelength of the recorded wavefield.
A field test was carried out in Oman in April 1998. With a lack of distinct P‐ and S‐waves in the data, the technique was instead evaluated on the airwave‐induced ground motion. The airwave arrival was found to consist mainly of vertical motion that decays with depth. The wavefield separation technique was successfully tested on this arrival.</description><subject>Arrivals</subject><subject>Decay</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes, seismology</subject><subject>Exact sciences and technology</subject><subject>Field tests</subject><subject>Ground motion</subject><subject>Internal geophysics</subject><subject>Mathematical analysis</subject><subject>Recording</subject><subject>Separation</subject><subject>Wavelengths</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkMFu1DAQhi1UJLYLNx4gBw4cCPV4HDs-VhVNkZZFoKKVuFheZwKGbLzYSaFvT5atWk5wmpHm-36NfsaeA38NXJgzMMY0Kw5cavGILcBIWdac6xO24NzMu9DqCTvN-RvnHDnCgq037oa6QH1bZNq75MYQh2LKYfhSuOIm9tOOijbkMYXt9OcWu2L8mogKH3f7ONAwFol8TO2s5Kfscef6TM_u5pJ9unxzfXFVrt43by_OV6WXUstSQge4FXrrZQsgDG_rzhE45ZRCaqXHVkNXK9wqLb3hwgEZEk5pgV5VNS7Zy2PuPsUfE-XR7kL21PduoDhlC1oJkBIr83-0Qm7qCg3M6Ksj6lPMOVFn9ynsXLq1wO2hYft3wzP-4i7ZZe_6LrnBh_zgGImoDg-II_Yz9HT7z0jbfFyBQCFnqTxKc_X0615y6btVGnVlN-vG4vVV_aEy7-xn_A3Hu5fX</recordid><startdate>19990915</startdate><enddate>19990915</enddate><creator>Robertsson, Johan O. A.</creator><creator>Muyzert, Everhard</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>19990915</creationdate><title>Wavefield separation using a volume distribution of three component recordings</title><author>Robertsson, Johan O. A. ; Muyzert, Everhard</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4474-41f13b27bc4d11290d8fae1a6a663ed4c3d71f863b674c902a1e9e2a6723c6583</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Arrivals</topic><topic>Decay</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Earthquakes, seismology</topic><topic>Exact sciences and technology</topic><topic>Field tests</topic><topic>Ground motion</topic><topic>Internal geophysics</topic><topic>Mathematical analysis</topic><topic>Recording</topic><topic>Separation</topic><topic>Wavelengths</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Robertsson, Johan O. A.</creatorcontrib><creatorcontrib>Muyzert, Everhard</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Robertsson, Johan O. A.</au><au>Muyzert, Everhard</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Wavefield separation using a volume distribution of three component recordings</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1999-09-15</date><risdate>1999</risdate><volume>26</volume><issue>18</issue><spage>2821</spage><epage>2824</epage><pages>2821-2824</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>By making multiple three component (3C) measurements around a volume so that the rate of change of the wavefield in all directions can be estimated, it is possible to calculate the divergence and the curl of the wavefield which in turns corresponds to P‐ and S‐waves. The volume may be of arbitrary shape, but the equations for wavefield separation are simplified if the volume has a known shape such as that of a tetrahedron. The dimensions of the volume should be smaller than approximately one fifth of the minimum wavelength of the recorded wavefield.
A field test was carried out in Oman in April 1998. With a lack of distinct P‐ and S‐waves in the data, the technique was instead evaluated on the airwave‐induced ground motion. The airwave arrival was found to consist mainly of vertical motion that decays with depth. The wavefield separation technique was successfully tested on this arrival.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/1999GL010472</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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issn | 0094-8276 1944-8007 |
language | eng |
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source | Wiley-Blackwell AGU Digital Archive |
subjects | Arrivals Decay Earth sciences Earth, ocean, space Earthquakes, seismology Exact sciences and technology Field tests Ground motion Internal geophysics Mathematical analysis Recording Separation Wavelengths |
title | Wavefield separation using a volume distribution of three component recordings |
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