Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram
This study investigates method of producing non-uniform support acceleration in actual site condition. Factors affecting the non-uniform excitation of topographic site include time delay between the arrival time of incident wave at the canyon floor and any particular point at higher elevation, causi...
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Iranian Society of Structrual Engineering (ISSE)
2020
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oai:doaj.org-article:8aa3146fd506432d84d092ef263d463b2021-11-08T15:53:21ZGeneration of Non-uniform support accelerations of topographic site using one recorded accelerogram2476-39772538-261610.22065/jsce.2018.121279.1487https://doaj.org/article/8aa3146fd506432d84d092ef263d463b2020-09-01T00:00:00Zhttps://www.jsce.ir/article_73685_adf18e7a15bd0bd5f0f85fc186e087ff.pdfhttps://doaj.org/toc/2476-3977https://doaj.org/toc/2538-2616This study investigates method of producing non-uniform support acceleration in actual site condition. Factors affecting the non-uniform excitation of topographic site include time delay between the arrival time of incident wave at the canyon floor and any particular point at higher elevation, causing phase difference. Another important factor in generating non-uniform accelerations is the topography amplification. Therefore, in the present study, two dimensional models of a canyon site subjected to Ricker wave with different predominant frequencies, shear wave velocities, shape ratios have been developed and the results of boundary element analyses in time domain (HYBRID code) were obtained in different elevations on the canyon surface. Then, by conducting a series of statistical analyses (Symbolic Regression and Genetic Programming) on the results from numerous presumed cases, the relationships for calculating the time delay between support responses of V-shaped canyons was obtained. To verify the accuracy of the proposed relationships, the results were compared with the records from Pacoima dam site during two different earthquakes and good agreement of the results was observed. Eventually, by implementing the presented relationships into random vibration method, non-uniform acceleration of the site was simulated. The results indicate that the proposed relationships have an appropriate level of accuracy to calculate time delay on the V-shaped canyons.Mohsen IsariReza TarinejadAbdullah Sohrabi-BidarSeyed Amir AlaviIranian Society of Structrual Engineering (ISSE)articlenon-uniform excitationsite effecttime delayamplificationboundary elementBridge engineeringTG1-470Building constructionTH1-9745FAJournal of Structural and Construction Engineering, Vol 7, Iss 3, Pp 193-213 (2020) |
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non-uniform excitation site effect time delay amplification boundary element Bridge engineering TG1-470 Building construction TH1-9745 |
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non-uniform excitation site effect time delay amplification boundary element Bridge engineering TG1-470 Building construction TH1-9745 Mohsen Isari Reza Tarinejad Abdullah Sohrabi-Bidar Seyed Amir Alavi Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
description |
This study investigates method of producing non-uniform support acceleration in actual site condition. Factors affecting the non-uniform excitation of topographic site include time delay between the arrival time of incident wave at the canyon floor and any particular point at higher elevation, causing phase difference. Another important factor in generating non-uniform accelerations is the topography amplification. Therefore, in the present study, two dimensional models of a canyon site subjected to Ricker wave with different predominant frequencies, shear wave velocities, shape ratios have been developed and the results of boundary element analyses in time domain (HYBRID code) were obtained in different elevations on the canyon surface. Then, by conducting a series of statistical analyses (Symbolic Regression and Genetic Programming) on the results from numerous presumed cases, the relationships for calculating the time delay between support responses of V-shaped canyons was obtained. To verify the accuracy of the proposed relationships, the results were compared with the records from Pacoima dam site during two different earthquakes and good agreement of the results was observed. Eventually, by implementing the presented relationships into random vibration method, non-uniform acceleration of the site was simulated. The results indicate that the proposed relationships have an appropriate level of accuracy to calculate time delay on the V-shaped canyons. |
format |
article |
author |
Mohsen Isari Reza Tarinejad Abdullah Sohrabi-Bidar Seyed Amir Alavi |
author_facet |
Mohsen Isari Reza Tarinejad Abdullah Sohrabi-Bidar Seyed Amir Alavi |
author_sort |
Mohsen Isari |
title |
Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
title_short |
Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
title_full |
Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
title_fullStr |
Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
title_full_unstemmed |
Generation of Non-uniform support accelerations of topographic site using one recorded accelerogram |
title_sort |
generation of non-uniform support accelerations of topographic site using one recorded accelerogram |
publisher |
Iranian Society of Structrual Engineering (ISSE) |
publishDate |
2020 |
url |
https://doaj.org/article/8aa3146fd506432d84d092ef263d463b |
work_keys_str_mv |
AT mohsenisari generationofnonuniformsupportaccelerationsoftopographicsiteusingonerecordedaccelerogram AT rezatarinejad generationofnonuniformsupportaccelerationsoftopographicsiteusingonerecordedaccelerogram AT abdullahsohrabibidar generationofnonuniformsupportaccelerationsoftopographicsiteusingonerecordedaccelerogram AT seyedamiralavi generationofnonuniformsupportaccelerationsoftopographicsiteusingonerecordedaccelerogram |
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1718441582274805760 |