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A split Hopkinson pressure bar for experimental investigation of dynamic pulverization under very high strain rates
Off-fault damage or pulverized rocks found in large-scale strike–slip faults are of great interest in earthquake research. In order to experimentally investigate rock pulverization, we developed a split Hopkinson pressure bar with compact dimensions and high-speed imaging. The developed experimental...
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Published in: | Review of scientific instruments 2023-09, Vol.94 (9) |
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creator | Jayawickrama, Eranga Gayanath Sekiguchi, Takuma Muto, Jun Sawa, Sando Nagahama, Hiroyuki Kono, Yoshio Bae, Kyung-Oh Shin, Hyung-Seop |
description | Off-fault damage or pulverized rocks found in large-scale strike–slip faults are of great interest in earthquake research. In order to experimentally investigate rock pulverization, we developed a split Hopkinson pressure bar with compact dimensions and high-speed imaging. The developed experimental setup is capable of generating very high strain rates up to 1320 s−1 with the satisfaction of stress equilibrium, which are essential to reproduce the dynamic pulverization observed in nature and obtain dynamic stress–strain responses accurately. High-speed imaging revealed that cracks initiate and propagate along the grain boundaries at very high speeds, while the dynamic stress–strain response suggested that energy dissipated into the fracture increases with stronger impacts. In addition, we show that the apparatus is capable of producing particle size distributions partly similar to those in naturally pulverized rocks of large-scale strike–slip faults. Thus, our developed system with compact dimensions opens new ways to understand the dynamics of the rock pulverization in off-fault regions of large-scale strike–slip faults. |
doi_str_mv | 10.1063/5.0151448 |
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In order to experimentally investigate rock pulverization, we developed a split Hopkinson pressure bar with compact dimensions and high-speed imaging. The developed experimental setup is capable of generating very high strain rates up to 1320 s−1 with the satisfaction of stress equilibrium, which are essential to reproduce the dynamic pulverization observed in nature and obtain dynamic stress–strain responses accurately. High-speed imaging revealed that cracks initiate and propagate along the grain boundaries at very high speeds, while the dynamic stress–strain response suggested that energy dissipated into the fracture increases with stronger impacts. In addition, we show that the apparatus is capable of producing particle size distributions partly similar to those in naturally pulverized rocks of large-scale strike–slip faults. 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In order to experimentally investigate rock pulverization, we developed a split Hopkinson pressure bar with compact dimensions and high-speed imaging. The developed experimental setup is capable of generating very high strain rates up to 1320 s−1 with the satisfaction of stress equilibrium, which are essential to reproduce the dynamic pulverization observed in nature and obtain dynamic stress–strain responses accurately. High-speed imaging revealed that cracks initiate and propagate along the grain boundaries at very high speeds, while the dynamic stress–strain response suggested that energy dissipated into the fracture increases with stronger impacts. In addition, we show that the apparatus is capable of producing particle size distributions partly similar to those in naturally pulverized rocks of large-scale strike–slip faults. Thus, our developed system with compact dimensions opens new ways to understand the dynamics of the rock pulverization in off-fault regions of large-scale strike–slip faults.</description><subject>Earthquake damage</subject><subject>Fault lines</subject><subject>Faults</subject><subject>Geological faults</subject><subject>Grain boundaries</subject><subject>High speed</subject><subject>High strain rate</subject><subject>Particle size distribution</subject><subject>Rocks</subject><subject>Scientific apparatus & instruments</subject><subject>Slip</subject><subject>Split Hopkinson pressure bars</subject><issn>0034-6748</issn><issn>1089-7623</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp90EFLwzAUB_AgCs7pwW8Q8KJC50uapO1xDHXCwIueS9qmW2aX1CQdzk9v3Hby4Ls8eO_H4_FH6JrAhIBIH_gECCeM5SdoRCAvkkzQ9BSNAFKWiIzl5-jC-zXE4oSMkJ9i33c64LntP7Tx1uDeKe8Hp3AlHW6tw-qrV05vlAmyw9pslQ96KYOO1ra42Rm50TXuh24b2fdhMZhGORwHO7zSyxX2wUltsJNB-Ut01srOq6tjH6P3p8e32TxZvD6_zKaLpKY5D0khpaC0YawFAkSxghc1pUKAqAgwWtWZ5HGR8TqrUpUCBajSgucgGtkKIdMxuj3c7Z39HOLX5Ub7WnWdNMoOvqS5EJkAmolIb_7QtR2cid_tFeGcpjyqu4OqnfXeqbbsYy7S7UoC5W_8JS-P8Ud7f7C-1mGfyT_4B5t4hMU</recordid><startdate>20230901</startdate><enddate>20230901</enddate><creator>Jayawickrama, Eranga Gayanath</creator><creator>Sekiguchi, Takuma</creator><creator>Muto, Jun</creator><creator>Sawa, Sando</creator><creator>Nagahama, Hiroyuki</creator><creator>Kono, Yoshio</creator><creator>Bae, Kyung-Oh</creator><creator>Shin, Hyung-Seop</creator><general>American Institute of Physics</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-4922-2427</orcidid><orcidid>https://orcid.org/0000-0002-7945-5870</orcidid><orcidid>https://orcid.org/0009-0001-0761-2822</orcidid><orcidid>https://orcid.org/0000-0001-9633-5179</orcidid><orcidid>https://orcid.org/0009-0005-2446-5114</orcidid><orcidid>https://orcid.org/0000-0001-8493-4051</orcidid><orcidid>https://orcid.org/0000-0002-3645-9505</orcidid><orcidid>https://orcid.org/0000-0001-5916-7524</orcidid></search><sort><creationdate>20230901</creationdate><title>A split Hopkinson pressure bar for experimental investigation of dynamic pulverization under very high strain rates</title><author>Jayawickrama, Eranga Gayanath ; Sekiguchi, Takuma ; Muto, Jun ; Sawa, Sando ; Nagahama, Hiroyuki ; Kono, Yoshio ; Bae, Kyung-Oh ; Shin, Hyung-Seop</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c285t-9aa622d44f0101e4959c226606b1042bc7a510175c7b3e30200b395806daf66a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Earthquake damage</topic><topic>Fault lines</topic><topic>Faults</topic><topic>Geological faults</topic><topic>Grain boundaries</topic><topic>High speed</topic><topic>High strain rate</topic><topic>Particle size distribution</topic><topic>Rocks</topic><topic>Scientific apparatus & instruments</topic><topic>Slip</topic><topic>Split Hopkinson pressure bars</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Jayawickrama, Eranga Gayanath</creatorcontrib><creatorcontrib>Sekiguchi, Takuma</creatorcontrib><creatorcontrib>Muto, Jun</creatorcontrib><creatorcontrib>Sawa, Sando</creatorcontrib><creatorcontrib>Nagahama, Hiroyuki</creatorcontrib><creatorcontrib>Kono, Yoshio</creatorcontrib><creatorcontrib>Bae, Kyung-Oh</creatorcontrib><creatorcontrib>Shin, Hyung-Seop</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>MEDLINE - Academic</collection><jtitle>Review of scientific instruments</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Jayawickrama, Eranga Gayanath</au><au>Sekiguchi, Takuma</au><au>Muto, Jun</au><au>Sawa, Sando</au><au>Nagahama, Hiroyuki</au><au>Kono, Yoshio</au><au>Bae, Kyung-Oh</au><au>Shin, Hyung-Seop</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A split Hopkinson pressure bar for experimental investigation of dynamic pulverization under very high strain rates</atitle><jtitle>Review of scientific instruments</jtitle><date>2023-09-01</date><risdate>2023</risdate><volume>94</volume><issue>9</issue><issn>0034-6748</issn><eissn>1089-7623</eissn><coden>RSINAK</coden><abstract>Off-fault damage or pulverized rocks found in large-scale strike–slip faults are of great interest in earthquake research. In order to experimentally investigate rock pulverization, we developed a split Hopkinson pressure bar with compact dimensions and high-speed imaging. The developed experimental setup is capable of generating very high strain rates up to 1320 s−1 with the satisfaction of stress equilibrium, which are essential to reproduce the dynamic pulverization observed in nature and obtain dynamic stress–strain responses accurately. High-speed imaging revealed that cracks initiate and propagate along the grain boundaries at very high speeds, while the dynamic stress–strain response suggested that energy dissipated into the fracture increases with stronger impacts. In addition, we show that the apparatus is capable of producing particle size distributions partly similar to those in naturally pulverized rocks of large-scale strike–slip faults. Thus, our developed system with compact dimensions opens new ways to understand the dynamics of the rock pulverization in off-fault regions of large-scale strike–slip faults.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/5.0151448</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-4922-2427</orcidid><orcidid>https://orcid.org/0000-0002-7945-5870</orcidid><orcidid>https://orcid.org/0009-0001-0761-2822</orcidid><orcidid>https://orcid.org/0000-0001-9633-5179</orcidid><orcidid>https://orcid.org/0009-0005-2446-5114</orcidid><orcidid>https://orcid.org/0000-0001-8493-4051</orcidid><orcidid>https://orcid.org/0000-0002-3645-9505</orcidid><orcidid>https://orcid.org/0000-0001-5916-7524</orcidid></addata></record> |
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subjects | Earthquake damage Fault lines Faults Geological faults Grain boundaries High speed High strain rate Particle size distribution Rocks Scientific apparatus & instruments Slip Split Hopkinson pressure bars |
title | A split Hopkinson pressure bar for experimental investigation of dynamic pulverization under very high strain rates |
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