Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K
The elastic wave velocities of polycrystalline Mj 80 Py 20 garnet along the majorite–pyrope system have been measured at pressures up to 21 GPa and temperatures up to 2,000 K using ultrasonic interferometry in conjunction with in situ X-ray diffraction techniques in a Kawai-type multi-anvil apparatu...
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| Veröffentlicht in: | Physics and chemistry of minerals 2015-03, Vol.42 (3), p.213-222 |
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| creator | Liu, Zhaodong Irifune, Tetsuo Gréaux, Steeve Arimoto, Takeshi Shinmei, Toru Higo, Yuji |
| description | The elastic wave velocities of polycrystalline Mj
80
Py
20
garnet along the majorite–pyrope system have been measured at pressures up to 21 GPa and temperatures up to 2,000 K using ultrasonic interferometry in conjunction with in situ X-ray diffraction techniques in a Kawai-type multi-anvil apparatus. The elastic moduli of Mj
80
Py
20
garnet and their pressure and temperature derivatives are determined by a two-dimensional linear fitting of the present experimental data, yielding:
K
S
= 161.5 (7) GPa
, ∂K
S
/
∂P
= 4.42 (4)
, ∂K
S
/
∂T
= −0.0154 (2) GPa/K
, G
= 86.2 (2) GPa
, ∂G
/
∂P
= 1.28 (1)
, ∂G
/
∂T
= −0.0096 (5) GPa/K. The present results together with those of the studies on the majorite–pyrope solid solutions suggest the pressure and temperature derivatives of elastic moduli are insensitive to the majorite content in the majorite–pyrope system. The velocity gradients of the majoritic garnets in the majorite–pyrope system are 3 ~ 6 times lower than those required to account for the high seismic velocity gradients observed in the mantle transition zone. |
| doi_str_mv | 10.1007/s00269-014-0712-y |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2262059821</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2262059821</sourcerecordid><originalsourceid>FETCH-LOGICAL-c452t-2e27189b5f231eb113432fceee5dfbc6a897059dab40ce815514891b52498bd3</originalsourceid><addsrcrecordid>eNp1kLFOwzAQQC0EEqXwAWyWWDHcXeImGVFVCqKIDt0tx3GqVCEpdlqUv-m39MtwFSQmplveuzs9xm4RHhAgefQANMkEYCwgQRL9GRthHJEgIDxnI4hiEphkeMmuvN9AAKNEjthyVmvfVYZ_673le1u3pup63pZ829a9cb3vdF1XjeXvmxSWPQFfa9fYjnctJzwe5kvNdVNwugeA4-Html2Uuvb25neO2ep5tpq-iMXH_HX6tBAmltQJspRgmuWypAhtjhiFZ0tjrZVFmZuJTrMEZFboPAZjU5QS4zTDXFKcpXkRjdndsHbr2q-d9Z3atDvXhIuKaEJBTQkDhQNlXOu9s6XauupTu14hqFM3NXRTIYc6dVN9cGhwfGCbtXV_m_-XfgBQ9G82</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2262059821</pqid></control><display><type>article</type><title>Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K</title><source>SpringerLink Journals - AutoHoldings</source><creator>Liu, Zhaodong ; Irifune, Tetsuo ; Gréaux, Steeve ; Arimoto, Takeshi ; Shinmei, Toru ; Higo, Yuji</creator><creatorcontrib>Liu, Zhaodong ; Irifune, Tetsuo ; Gréaux, Steeve ; Arimoto, Takeshi ; Shinmei, Toru ; Higo, Yuji</creatorcontrib><description>The elastic wave velocities of polycrystalline Mj
80
Py
20
garnet along the majorite–pyrope system have been measured at pressures up to 21 GPa and temperatures up to 2,000 K using ultrasonic interferometry in conjunction with in situ X-ray diffraction techniques in a Kawai-type multi-anvil apparatus. The elastic moduli of Mj
80
Py
20
garnet and their pressure and temperature derivatives are determined by a two-dimensional linear fitting of the present experimental data, yielding:
K
S
= 161.5 (7) GPa
, ∂K
S
/
∂P
= 4.42 (4)
, ∂K
S
/
∂T
= −0.0154 (2) GPa/K
, G
= 86.2 (2) GPa
, ∂G
/
∂P
= 1.28 (1)
, ∂G
/
∂T
= −0.0096 (5) GPa/K. The present results together with those of the studies on the majorite–pyrope solid solutions suggest the pressure and temperature derivatives of elastic moduli are insensitive to the majorite content in the majorite–pyrope system. The velocity gradients of the majoritic garnets in the majorite–pyrope system are 3 ~ 6 times lower than those required to account for the high seismic velocity gradients observed in the mantle transition zone.</description><identifier>ISSN: 0342-1791</identifier><identifier>EISSN: 1432-2021</identifier><identifier>DOI: 10.1007/s00269-014-0712-y</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Crystallography and Scattering Methods ; Derivatives ; Earth and Environmental Science ; Earth Sciences ; Elastic waves ; Garnets ; Geochemistry ; Interferometry ; Magnesium aluminum silicates ; Mineral Resources ; Mineralogy ; Modulus of elasticity ; Original Paper ; Polycrystals ; Solid solutions ; Transition zone ; Velocity gradient ; Wave velocity ; X-ray diffraction</subject><ispartof>Physics and chemistry of minerals, 2015-03, Vol.42 (3), p.213-222</ispartof><rights>Springer-Verlag Berlin Heidelberg 2014</rights><rights>Physics and Chemistry of Minerals is a copyright of Springer, (2014). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c452t-2e27189b5f231eb113432fceee5dfbc6a897059dab40ce815514891b52498bd3</citedby><cites>FETCH-LOGICAL-c452t-2e27189b5f231eb113432fceee5dfbc6a897059dab40ce815514891b52498bd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00269-014-0712-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00269-014-0712-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Liu, Zhaodong</creatorcontrib><creatorcontrib>Irifune, Tetsuo</creatorcontrib><creatorcontrib>Gréaux, Steeve</creatorcontrib><creatorcontrib>Arimoto, Takeshi</creatorcontrib><creatorcontrib>Shinmei, Toru</creatorcontrib><creatorcontrib>Higo, Yuji</creatorcontrib><title>Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K</title><title>Physics and chemistry of minerals</title><addtitle>Phys Chem Minerals</addtitle><description>The elastic wave velocities of polycrystalline Mj
80
Py
20
garnet along the majorite–pyrope system have been measured at pressures up to 21 GPa and temperatures up to 2,000 K using ultrasonic interferometry in conjunction with in situ X-ray diffraction techniques in a Kawai-type multi-anvil apparatus. The elastic moduli of Mj
80
Py
20
garnet and their pressure and temperature derivatives are determined by a two-dimensional linear fitting of the present experimental data, yielding:
K
S
= 161.5 (7) GPa
, ∂K
S
/
∂P
= 4.42 (4)
, ∂K
S
/
∂T
= −0.0154 (2) GPa/K
, G
= 86.2 (2) GPa
, ∂G
/
∂P
= 1.28 (1)
, ∂G
/
∂T
= −0.0096 (5) GPa/K. The present results together with those of the studies on the majorite–pyrope solid solutions suggest the pressure and temperature derivatives of elastic moduli are insensitive to the majorite content in the majorite–pyrope system. The velocity gradients of the majoritic garnets in the majorite–pyrope system are 3 ~ 6 times lower than those required to account for the high seismic velocity gradients observed in the mantle transition zone.</description><subject>Crystallography and Scattering Methods</subject><subject>Derivatives</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Elastic waves</subject><subject>Garnets</subject><subject>Geochemistry</subject><subject>Interferometry</subject><subject>Magnesium aluminum silicates</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Modulus of elasticity</subject><subject>Original Paper</subject><subject>Polycrystals</subject><subject>Solid solutions</subject><subject>Transition zone</subject><subject>Velocity gradient</subject><subject>Wave velocity</subject><subject>X-ray diffraction</subject><issn>0342-1791</issn><issn>1432-2021</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNp1kLFOwzAQQC0EEqXwAWyWWDHcXeImGVFVCqKIDt0tx3GqVCEpdlqUv-m39MtwFSQmplveuzs9xm4RHhAgefQANMkEYCwgQRL9GRthHJEgIDxnI4hiEphkeMmuvN9AAKNEjthyVmvfVYZ_673le1u3pup63pZ829a9cb3vdF1XjeXvmxSWPQFfa9fYjnctJzwe5kvNdVNwugeA4-Html2Uuvb25neO2ep5tpq-iMXH_HX6tBAmltQJspRgmuWypAhtjhiFZ0tjrZVFmZuJTrMEZFboPAZjU5QS4zTDXFKcpXkRjdndsHbr2q-d9Z3atDvXhIuKaEJBTQkDhQNlXOu9s6XauupTu14hqFM3NXRTIYc6dVN9cGhwfGCbtXV_m_-XfgBQ9G82</recordid><startdate>20150301</startdate><enddate>20150301</enddate><creator>Liu, Zhaodong</creator><creator>Irifune, Tetsuo</creator><creator>Gréaux, Steeve</creator><creator>Arimoto, Takeshi</creator><creator>Shinmei, Toru</creator><creator>Higo, Yuji</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>AFKRA</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>KB.</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope></search><sort><creationdate>20150301</creationdate><title>Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K</title><author>Liu, Zhaodong ; Irifune, Tetsuo ; Gréaux, Steeve ; Arimoto, Takeshi ; Shinmei, Toru ; Higo, Yuji</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c452t-2e27189b5f231eb113432fceee5dfbc6a897059dab40ce815514891b52498bd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Crystallography and Scattering Methods</topic><topic>Derivatives</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Elastic waves</topic><topic>Garnets</topic><topic>Geochemistry</topic><topic>Interferometry</topic><topic>Magnesium aluminum silicates</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Modulus of elasticity</topic><topic>Original Paper</topic><topic>Polycrystals</topic><topic>Solid solutions</topic><topic>Transition zone</topic><topic>Velocity gradient</topic><topic>Wave velocity</topic><topic>X-ray diffraction</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Zhaodong</creatorcontrib><creatorcontrib>Irifune, Tetsuo</creatorcontrib><creatorcontrib>Gréaux, Steeve</creatorcontrib><creatorcontrib>Arimoto, Takeshi</creatorcontrib><creatorcontrib>Shinmei, Toru</creatorcontrib><creatorcontrib>Higo, Yuji</creatorcontrib><collection>CrossRef</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>Materials Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><jtitle>Physics and chemistry of minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Zhaodong</au><au>Irifune, Tetsuo</au><au>Gréaux, Steeve</au><au>Arimoto, Takeshi</au><au>Shinmei, Toru</au><au>Higo, Yuji</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K</atitle><jtitle>Physics and chemistry of minerals</jtitle><stitle>Phys Chem Minerals</stitle><date>2015-03-01</date><risdate>2015</risdate><volume>42</volume><issue>3</issue><spage>213</spage><epage>222</epage><pages>213-222</pages><issn>0342-1791</issn><eissn>1432-2021</eissn><abstract>The elastic wave velocities of polycrystalline Mj
80
Py
20
garnet along the majorite–pyrope system have been measured at pressures up to 21 GPa and temperatures up to 2,000 K using ultrasonic interferometry in conjunction with in situ X-ray diffraction techniques in a Kawai-type multi-anvil apparatus. The elastic moduli of Mj
80
Py
20
garnet and their pressure and temperature derivatives are determined by a two-dimensional linear fitting of the present experimental data, yielding:
K
S
= 161.5 (7) GPa
, ∂K
S
/
∂P
= 4.42 (4)
, ∂K
S
/
∂T
= −0.0154 (2) GPa/K
, G
= 86.2 (2) GPa
, ∂G
/
∂P
= 1.28 (1)
, ∂G
/
∂T
= −0.0096 (5) GPa/K. The present results together with those of the studies on the majorite–pyrope solid solutions suggest the pressure and temperature derivatives of elastic moduli are insensitive to the majorite content in the majorite–pyrope system. The velocity gradients of the majoritic garnets in the majorite–pyrope system are 3 ~ 6 times lower than those required to account for the high seismic velocity gradients observed in the mantle transition zone.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00269-014-0712-y</doi><tpages>10</tpages></addata></record> |
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| subjects | Crystallography and Scattering Methods Derivatives Earth and Environmental Science Earth Sciences Elastic waves Garnets Geochemistry Interferometry Magnesium aluminum silicates Mineral Resources Mineralogy Modulus of elasticity Original Paper Polycrystals Solid solutions Transition zone Velocity gradient Wave velocity X-ray diffraction |
| title | Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K |
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