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Shock melting and the hcp-bcc phase boundary of Mg under dynamic loading
The high-temperature and high-pressure response of magnesium has been investigated through shock-release experiments performed up to shock melting. The longitudinal and bulk sound speeds of Mg are reported along the Hugoniot from 25 to 56 GPa and used to determine the elastic properties and Grüneise...
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Published in: | Physical review. B 2021-10, Vol.104 (14), Article 144106 |
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description | The high-temperature and high-pressure response of magnesium has been investigated through shock-release experiments performed up to shock melting. The longitudinal and bulk sound speeds of Mg are reported along the Hugoniot from 25 to 56 GPa and used to determine the elastic properties and Grüneisen parameter. The hexagonal close-packed (hcp)–body-centered cubic (bcc) phase transition is marked by a reduction in the determined shear wave speed. Thermal softening is observed to begin between 40 and 44 GPa, with incipient melt at 55.5 GPa, in close agreement with previous diffraction measurements under laser shock loading. Examination of the release profiles showed that two different responses were observed, depending on the peak stress. When plotted in a stress-energy phase diagram, the two responses are observed to form separate lines that intersect the static hcp-bcc phase transition and incipient melt. The results indicate that the hcp-bcc transition occurs on the Hugoniot at 28.4 GPa and place the hcp-bcc-liquid triple point ∼20 GPa. A multiphase equation of state is developed which places the melt boundary below the previously reported static measurements. |
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T. ; Jensen, B. J. ; Crockett, S. D.</creator><creatorcontrib>Beason, M. T. ; Jensen, B. J. ; Crockett, S. D.</creatorcontrib><description>The high-temperature and high-pressure response of magnesium has been investigated through shock-release experiments performed up to shock melting. The longitudinal and bulk sound speeds of Mg are reported along the Hugoniot from 25 to 56 GPa and used to determine the elastic properties and Grüneisen parameter. The hexagonal close-packed (hcp)–body-centered cubic (bcc) phase transition is marked by a reduction in the determined shear wave speed. Thermal softening is observed to begin between 40 and 44 GPa, with incipient melt at 55.5 GPa, in close agreement with previous diffraction measurements under laser shock loading. Examination of the release profiles showed that two different responses were observed, depending on the peak stress. When plotted in a stress-energy phase diagram, the two responses are observed to form separate lines that intersect the static hcp-bcc phase transition and incipient melt. The results indicate that the hcp-bcc transition occurs on the Hugoniot at 28.4 GPa and place the hcp-bcc-liquid triple point ∼20 GPa. A multiphase equation of state is developed which places the melt boundary below the previously reported static measurements.</description><identifier>ISSN: 2469-9950</identifier><identifier>EISSN: 2469-9969</identifier><identifier>DOI: 10.1103/PhysRevB.104.144106</identifier><language>eng</language><publisher>College Park: American Physical Society</publisher><subject>Dynamic loads ; Elastic properties ; Equations of state ; Gruneisen parameter ; High temperature ; Magnesium ; Phase diagrams ; Phase transitions ; Shock loading</subject><ispartof>Physical review. 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B</title><description>The high-temperature and high-pressure response of magnesium has been investigated through shock-release experiments performed up to shock melting. The longitudinal and bulk sound speeds of Mg are reported along the Hugoniot from 25 to 56 GPa and used to determine the elastic properties and Grüneisen parameter. The hexagonal close-packed (hcp)–body-centered cubic (bcc) phase transition is marked by a reduction in the determined shear wave speed. Thermal softening is observed to begin between 40 and 44 GPa, with incipient melt at 55.5 GPa, in close agreement with previous diffraction measurements under laser shock loading. Examination of the release profiles showed that two different responses were observed, depending on the peak stress. When plotted in a stress-energy phase diagram, the two responses are observed to form separate lines that intersect the static hcp-bcc phase transition and incipient melt. The results indicate that the hcp-bcc transition occurs on the Hugoniot at 28.4 GPa and place the hcp-bcc-liquid triple point ∼20 GPa. A multiphase equation of state is developed which places the melt boundary below the previously reported static measurements.</description><subject>Dynamic loads</subject><subject>Elastic properties</subject><subject>Equations of state</subject><subject>Gruneisen parameter</subject><subject>High temperature</subject><subject>Magnesium</subject><subject>Phase diagrams</subject><subject>Phase transitions</subject><subject>Shock loading</subject><issn>2469-9950</issn><issn>2469-9969</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNo9kEtLAzEUhYMoWGp_gZuA66k378lSi1qhovhYhySTdFrbyTiZFvrvHam6ug_OuYf7IXRJYEoIsOuX-pBfw_52SoBPCecE5AkaUS51obXUp_-9gHM0yXkNAESCVqBHaP5WJ_-Jt2HTr5oltk2F-zrg2reF8x63tc0Bu7RrKtsdcIr4aYmHIXS4OjR2u_J4k2w1WC_QWbSbHCa_dYw-7u_eZ_Ni8fzwOLtZFJ4q1RciRhdjSakIStgKQNOSEcos4-CIq5SjQRMrnXWOBAe6IoorVoqSU2BesDG6Ot5tu_S1C7k367TrmiHSUKGFFIpROajYUeW7lHMXomm71XZ4wRAwP9TMH7Vhwc2RGvsGl9BgVw</recordid><startdate>20211001</startdate><enddate>20211001</enddate><creator>Beason, M. 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D.</creatorcontrib><collection>CrossRef</collection><collection>Engineered Materials Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Materials Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Physical review. B</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Beason, M. T.</au><au>Jensen, B. J.</au><au>Crockett, S. D.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Shock melting and the hcp-bcc phase boundary of Mg under dynamic loading</atitle><jtitle>Physical review. 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When plotted in a stress-energy phase diagram, the two responses are observed to form separate lines that intersect the static hcp-bcc phase transition and incipient melt. The results indicate that the hcp-bcc transition occurs on the Hugoniot at 28.4 GPa and place the hcp-bcc-liquid triple point ∼20 GPa. A multiphase equation of state is developed which places the melt boundary below the previously reported static measurements.</abstract><cop>College Park</cop><pub>American Physical Society</pub><doi>10.1103/PhysRevB.104.144106</doi><orcidid>https://orcid.org/0000-0002-2056-7456</orcidid><orcidid>https://orcid.org/0000-0001-7460-5772</orcidid></addata></record> |
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subjects | Dynamic loads Elastic properties Equations of state Gruneisen parameter High temperature Magnesium Phase diagrams Phase transitions Shock loading |
title | Shock melting and the hcp-bcc phase boundary of Mg under dynamic loading |
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