Ground motion prediction equation ("attenuation relationship") for inelastic response spectra
This paper presents the process and fundamental results of a comprehensive ground motion prediction equation (GMPE, or "attenuation" relationship) developed for inelastic response spectra. We used over 3,100 horizontal ground motions recorded in 64 earthquakes with moment magnitudes rangin...
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| Veröffentlicht in: | Earthquake spectra 2010-02, Vol.26 (1), p.1-23 |
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| container_title | Earthquake spectra |
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| creator | Bozorgnia, Yousef Hachem, Mahmoud M Campbell, Kenneth W |
| description | This paper presents the process and fundamental results of a comprehensive ground motion prediction equation (GMPE, or "attenuation" relationship) developed for inelastic response spectra. We used over 3,100 horizontal ground motions recorded in 64 earthquakes with moment magnitudes ranging from 4.3-7.9 and rupture distances ranging from 0.1-199 km. For each record, we computed inelastic spectra for ductility ranging from one (elastic response) to eight. Our GMPE correlates inelastic spectral ordinates to earthquake magnitude, site-to-source distance, fault mechanism, local soil properties, and basin effects. The developed GMPE is used in both deterministic and probabilistic hazard analyses to directly generate inelastic spectra. This is in contrast to developing "attenuation" relationships for elastic response spectra, carrying out a hazard analysis, and subsequently adopting approximate rules to derive inelastic response from elastic spectra. |
| doi_str_mv | 10.1193/1.3281182 |
| format | Article |
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We used over 3,100 horizontal ground motions recorded in 64 earthquakes with moment magnitudes ranging from 4.3-7.9 and rupture distances ranging from 0.1-199 km. For each record, we computed inelastic spectra for ductility ranging from one (elastic response) to eight. Our GMPE correlates inelastic spectral ordinates to earthquake magnitude, site-to-source distance, fault mechanism, local soil properties, and basin effects. The developed GMPE is used in both deterministic and probabilistic hazard analyses to directly generate inelastic spectra. This is in contrast to developing "attenuation" relationships for elastic response spectra, carrying out a hazard analysis, and subsequently adopting approximate rules to derive inelastic response from elastic spectra.</description><identifier>ISSN: 8755-2930</identifier><identifier>EISSN: 1944-8201</identifier><identifier>DOI: 10.1193/1.3281182</identifier><identifier>CODEN: EASPEF</identifier><language>eng</language><publisher>Oakland, CA: Earthquake Engineering Research Institute</publisher><subject>acceleration ; attenuation ; design ; ductility ; Earth sciences ; Earth, ocean, space ; earthquake prediction ; earthquakes ; Earthquakes, seismology ; Engineering and environment geology. 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We used over 3,100 horizontal ground motions recorded in 64 earthquakes with moment magnitudes ranging from 4.3-7.9 and rupture distances ranging from 0.1-199 km. For each record, we computed inelastic spectra for ductility ranging from one (elastic response) to eight. Our GMPE correlates inelastic spectral ordinates to earthquake magnitude, site-to-source distance, fault mechanism, local soil properties, and basin effects. The developed GMPE is used in both deterministic and probabilistic hazard analyses to directly generate inelastic spectra. This is in contrast to developing "attenuation" relationships for elastic response spectra, carrying out a hazard analysis, and subsequently adopting approximate rules to derive inelastic response from elastic spectra.</description><subject>acceleration</subject><subject>attenuation</subject><subject>design</subject><subject>ductility</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>earthquake prediction</subject><subject>earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Engineering and environment geology. Geothermics</subject><subject>equations</subject><subject>Exact sciences and technology</subject><subject>ground motion</subject><subject>Internal geophysics</subject><subject>magnitude</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>seismic response</subject><subject>seismic risk</subject><subject>Seismology</subject><subject>soils</subject><subject>statistical analysis</subject><issn>8755-2930</issn><issn>1944-8201</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNp9kclKBDEQhoMoOC4H36AR3JDWrN2Vo4gbDHjRo4RMplojPZ026UZ8ezMLHj3VX6kvlao_hBwxesWYFtfsSnBgDPgWmTAtZQmcsm0ygVqpkmtBd8leSp-UskpSOiFvDzGM3bxYhMGHrugjzr1bSfwa7UqcH9thwG6TRWxXIn34_viiaEIsfJfP0uBdLqY-l7BIPboh2gOy09g24eEm7pPX-7uX28dy-vzwdHszLa0ANpQSnKZWqQpmtebgKilqnAEFANGgVsCxqkCCYLOmmVs1sxXNYF6BOZCoxT45W_ftY_gaMQ1m4ZPDtrUdhjGZWgrOhYIqk6f_kpxJDapiGbxYgy6GlCI2po9-YeOPYdQsrTbMbKzO7MmmqU3Otk20nfPp70J-WmutlmNerrl3DMl57Bx-h9jOzWcYY5cNMvmzuKE1l6oWv_Jui-c</recordid><startdate>20100201</startdate><enddate>20100201</enddate><creator>Bozorgnia, Yousef</creator><creator>Hachem, Mahmoud M</creator><creator>Campbell, Kenneth W</creator><general>Earthquake Engineering Research Institute</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7T2</scope><scope>7U2</scope><scope>C1K</scope><scope>7SM</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20100201</creationdate><title>Ground motion prediction equation ("attenuation relationship") for inelastic response spectra</title><author>Bozorgnia, Yousef ; Hachem, Mahmoud M ; Campbell, Kenneth W</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a381t-48c90a5568b7928c6437eb808883fe9582e6684831bffda5ba607921641c84e93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>acceleration</topic><topic>attenuation</topic><topic>design</topic><topic>ductility</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>earthquake prediction</topic><topic>earthquakes</topic><topic>Earthquakes, seismology</topic><topic>Engineering and environment geology. Geothermics</topic><topic>equations</topic><topic>Exact sciences and technology</topic><topic>ground motion</topic><topic>Internal geophysics</topic><topic>magnitude</topic><topic>Natural hazards: prediction, damages, etc</topic><topic>seismic response</topic><topic>seismic risk</topic><topic>Seismology</topic><topic>soils</topic><topic>statistical analysis</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bozorgnia, Yousef</creatorcontrib><creatorcontrib>Hachem, Mahmoud M</creatorcontrib><creatorcontrib>Campbell, Kenneth W</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Health and Safety Science Abstracts (Full archive)</collection><collection>Safety Science and Risk</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Earthquake Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Earthquake spectra</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bozorgnia, Yousef</au><au>Hachem, Mahmoud M</au><au>Campbell, Kenneth W</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ground motion prediction equation ("attenuation relationship") for inelastic response spectra</atitle><jtitle>Earthquake spectra</jtitle><date>2010-02-01</date><risdate>2010</risdate><volume>26</volume><issue>1</issue><spage>1</spage><epage>23</epage><pages>1-23</pages><issn>8755-2930</issn><eissn>1944-8201</eissn><coden>EASPEF</coden><abstract>This paper presents the process and fundamental results of a comprehensive ground motion prediction equation (GMPE, or "attenuation" relationship) developed for inelastic response spectra. We used over 3,100 horizontal ground motions recorded in 64 earthquakes with moment magnitudes ranging from 4.3-7.9 and rupture distances ranging from 0.1-199 km. For each record, we computed inelastic spectra for ductility ranging from one (elastic response) to eight. Our GMPE correlates inelastic spectral ordinates to earthquake magnitude, site-to-source distance, fault mechanism, local soil properties, and basin effects. The developed GMPE is used in both deterministic and probabilistic hazard analyses to directly generate inelastic spectra. This is in contrast to developing "attenuation" relationships for elastic response spectra, carrying out a hazard analysis, and subsequently adopting approximate rules to derive inelastic response from elastic spectra.</abstract><cop>Oakland, CA</cop><pub>Earthquake Engineering Research Institute</pub><doi>10.1193/1.3281182</doi><tpages>23</tpages></addata></record> |
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| subjects | acceleration attenuation design ductility Earth sciences Earth, ocean, space earthquake prediction earthquakes Earthquakes, seismology Engineering and environment geology. Geothermics equations Exact sciences and technology ground motion Internal geophysics magnitude Natural hazards: prediction, damages, etc seismic response seismic risk Seismology soils statistical analysis |
| title | Ground motion prediction equation ("attenuation relationship") for inelastic response spectra |
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