Lattice dynamics and thermodynamic properties of (Mg,Fe2+)SiO3 postperovskite
Phonon dispersion relations and vibrational density of states of (Mg0.9375Fe0.0625)SiO3 postperovskite have been determined by direct first‐principles calculations of the dynamical matrix up to 150 GPa. Incorporation of iron in the postperovskite phase, irrespective of the two investigated configura...
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Veröffentlicht in: | Journal of Geophysical Research: Solid Earth 2011-08, Vol.116 (B8), p.n/a |
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description | Phonon dispersion relations and vibrational density of states of (Mg0.9375Fe0.0625)SiO3 postperovskite have been determined by direct first‐principles calculations of the dynamical matrix up to 150 GPa. Incorporation of iron in the postperovskite phase, irrespective of the two investigated configurations and the spin state, was found to decrease the acoustic phonon frequencies but to have a minor effect on the optic modes at high frequencies. The phonon dispersion curves exhibit negative phonon frequencies below 10 GPa when iron is incorporated in the high or low spin state and indicate unstable dynamic structures. Then, the calculated phonon frequencies of dynamically stable structures are used to determine vibrational contributions to the Helmholtz free energy within the quasi‐harmonic approximation. The high temperature equation of state and several thermodynamic properties are then derived for (Mg0.9375Fe0.0625)SiO3 postperovskite and compared with those of pure MgSiO3 postperovskite. The results show that a low concentration of iron, irrespective of high spin or low spin, in MgSiO3 postperovskite has a minor effect on the thermodynamic properties at pressure‐temperature conditions of the lowermost part of the Earth's mantle.
Key Points
Addition of Fe in the PPv phase decreases the acoustic phonon frequencies
Low concentration of Fe has a small influence on the thermodynamic properties |
doi_str_mv | 10.1029/2010JB008018 |
format | Article |
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Key Points
Addition of Fe in the PPv phase decreases the acoustic phonon frequencies
Low concentration of Fe has a small influence on the thermodynamic properties</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9313</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9356</identifier><identifier>DOI: 10.1029/2010JB008018</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Earth mantle ; Geophysics ; High temperature ; Iron ; Materials science ; postperovskite ; Thermodynamics</subject><ispartof>Journal of Geophysical Research: Solid Earth, 2011-08, Vol.116 (B8), p.n/a</ispartof><rights>Copyright 2011 by the American Geophysical Union.</rights><rights>Copyright 2011 by American Geophysical Union</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2010JB008018$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2010JB008018$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids></links><search><creatorcontrib>Metsue, Arnaud</creatorcontrib><creatorcontrib>Tsuchiya, Taku</creatorcontrib><title>Lattice dynamics and thermodynamic properties of (Mg,Fe2+)SiO3 postperovskite</title><title>Journal of Geophysical Research: Solid Earth</title><addtitle>J. Geophys. Res</addtitle><description>Phonon dispersion relations and vibrational density of states of (Mg0.9375Fe0.0625)SiO3 postperovskite have been determined by direct first‐principles calculations of the dynamical matrix up to 150 GPa. Incorporation of iron in the postperovskite phase, irrespective of the two investigated configurations and the spin state, was found to decrease the acoustic phonon frequencies but to have a minor effect on the optic modes at high frequencies. The phonon dispersion curves exhibit negative phonon frequencies below 10 GPa when iron is incorporated in the high or low spin state and indicate unstable dynamic structures. Then, the calculated phonon frequencies of dynamically stable structures are used to determine vibrational contributions to the Helmholtz free energy within the quasi‐harmonic approximation. The high temperature equation of state and several thermodynamic properties are then derived for (Mg0.9375Fe0.0625)SiO3 postperovskite and compared with those of pure MgSiO3 postperovskite. The results show that a low concentration of iron, irrespective of high spin or low spin, in MgSiO3 postperovskite has a minor effect on the thermodynamic properties at pressure‐temperature conditions of the lowermost part of the Earth's mantle.
Key Points
Addition of Fe in the PPv phase decreases the acoustic phonon frequencies
Low concentration of Fe has a small influence on the thermodynamic properties</description><subject>Earth mantle</subject><subject>Geophysics</subject><subject>High temperature</subject><subject>Iron</subject><subject>Materials science</subject><subject>postperovskite</subject><subject>Thermodynamics</subject><issn>0148-0227</issn><issn>2169-9313</issn><issn>2156-2202</issn><issn>2169-9356</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNpNkFtLAzEQhYMoWGrf_AGLT4quTu7ZR622WroWvCD4ErabVNPbrptU7b830iLOy8DMOTMfB6FDDOcYSHZBAMPgCkABVjuoRTAXKSFAdlELMFMpECL3Ucf7KcRiXDDALZQPixBcaROzXhYLV_qkWJokvNtmUW1HSd1UtW2Csz6pJslx_nbWs-T05NGNaFJXPsRl9elnLtgDtDcp5t52tr2Nnns3T93bdDjq33Uvh6kjguF0jDnPzLjElNOxgcyUtBACJpFJYkwyJjiW3ERIlZVQSma4VRYKlhljJ4bTNjra3I1oHyvrg55Wq2YZX2qlKFGMySyK6Eb05eZ2revGLYpmrTHo37z0_7z0oP9whYWUOLrSjcv5YL__XEUz00JSyfXLfV_nRA1e82uqFf0BeEFsQg</recordid><startdate>201108</startdate><enddate>201108</enddate><creator>Metsue, Arnaud</creator><creator>Tsuchiya, Taku</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>201108</creationdate><title>Lattice dynamics and thermodynamic properties of (Mg,Fe2+)SiO3 postperovskite</title><author>Metsue, Arnaud ; Tsuchiya, Taku</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-i2641-b1559dbc1353bd09dc3a660f56471129465175d04589c0c74d5e8e0a49ddefd53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Earth mantle</topic><topic>Geophysics</topic><topic>High temperature</topic><topic>Iron</topic><topic>Materials science</topic><topic>postperovskite</topic><topic>Thermodynamics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Metsue, Arnaud</creatorcontrib><creatorcontrib>Tsuchiya, Taku</creatorcontrib><collection>Istex</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of Geophysical Research: Solid Earth</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Metsue, Arnaud</au><au>Tsuchiya, Taku</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Lattice dynamics and thermodynamic properties of (Mg,Fe2+)SiO3 postperovskite</atitle><jtitle>Journal of Geophysical Research: Solid Earth</jtitle><addtitle>J. Geophys. Res</addtitle><date>2011-08</date><risdate>2011</risdate><volume>116</volume><issue>B8</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9313</issn><eissn>2156-2202</eissn><eissn>2169-9356</eissn><abstract>Phonon dispersion relations and vibrational density of states of (Mg0.9375Fe0.0625)SiO3 postperovskite have been determined by direct first‐principles calculations of the dynamical matrix up to 150 GPa. Incorporation of iron in the postperovskite phase, irrespective of the two investigated configurations and the spin state, was found to decrease the acoustic phonon frequencies but to have a minor effect on the optic modes at high frequencies. The phonon dispersion curves exhibit negative phonon frequencies below 10 GPa when iron is incorporated in the high or low spin state and indicate unstable dynamic structures. Then, the calculated phonon frequencies of dynamically stable structures are used to determine vibrational contributions to the Helmholtz free energy within the quasi‐harmonic approximation. The high temperature equation of state and several thermodynamic properties are then derived for (Mg0.9375Fe0.0625)SiO3 postperovskite and compared with those of pure MgSiO3 postperovskite. The results show that a low concentration of iron, irrespective of high spin or low spin, in MgSiO3 postperovskite has a minor effect on the thermodynamic properties at pressure‐temperature conditions of the lowermost part of the Earth's mantle.
Key Points
Addition of Fe in the PPv phase decreases the acoustic phonon frequencies
Low concentration of Fe has a small influence on the thermodynamic properties</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2010JB008018</doi><tpages>11</tpages></addata></record> |
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subjects | Earth mantle Geophysics High temperature Iron Materials science postperovskite Thermodynamics |
title | Lattice dynamics and thermodynamic properties of (Mg,Fe2+)SiO3 postperovskite |
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