Structure and nuclear density distribution in the cheralite—CaTh(PO4)2: studies of its behaviour under high pressure (36 GPa)
The crystal structure of the cheralite—CaTh(PO 4 ) 2 —has been revisited by neutron diffraction and its behaviour under high pressure investigated by X-ray diffraction up to 36 GPa. The neutron diffraction data at ambient pressure gave a more accurate determination of the Ca/Th cation position than...
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| Veröffentlicht in: | Physics and chemistry of minerals 2012-09, Vol.39 (8), p.685-692 |
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| creator | Raison, Philippe E. Heathman, Stephen Wallez, Gilles Zvoriste, Carmen E. Bykov, Denis Ménard, Gaël Suard, Emmanuelle Popa, Karin Dacheux, Nicolas Konings, Rudy J. M. Caciuffo, Roberto |
| description | The crystal structure of the cheralite—CaTh(PO
4
)
2
—has been revisited by neutron diffraction and its behaviour under high pressure investigated by X-ray diffraction up to 36 GPa. The neutron diffraction data at ambient pressure gave a more accurate determination of the Ca/Th cation position than previous XRD data, taking advantage that the neutron scattering lengths of calcium and thorium are of same order of magnitude. The nuclear density distribution was also determined using the maximum entropy method (MEM) confirming that the two cations are not located at the same position in the unit cell but are slightly displaced from one another along a specific direction in order to minimize the electrostatic repulsion with the surrounding phosphorus atoms. At high pressure, the compound did not show any phase transition or amorphization. From the evolution of the unit-cell volume as a function of the pressure, the zero-pressure bulk modulus B
0
and its pressure derivative B
0
′
have been determined by fitting the experimental compressibility curve to the Birch–Murnaghan equation of state. The results are B
0
= 140(2) GPa and B
0
′
= 4.4(4) GPa. |
| doi_str_mv | 10.1007/s00269-012-0522-z |
| format | Article |
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4
)
2
—has been revisited by neutron diffraction and its behaviour under high pressure investigated by X-ray diffraction up to 36 GPa. The neutron diffraction data at ambient pressure gave a more accurate determination of the Ca/Th cation position than previous XRD data, taking advantage that the neutron scattering lengths of calcium and thorium are of same order of magnitude. The nuclear density distribution was also determined using the maximum entropy method (MEM) confirming that the two cations are not located at the same position in the unit cell but are slightly displaced from one another along a specific direction in order to minimize the electrostatic repulsion with the surrounding phosphorus atoms. At high pressure, the compound did not show any phase transition or amorphization. From the evolution of the unit-cell volume as a function of the pressure, the zero-pressure bulk modulus B
0
and its pressure derivative B
0
′
have been determined by fitting the experimental compressibility curve to the Birch–Murnaghan equation of state. The results are B
0
= 140(2) GPa and B
0
′
= 4.4(4) GPa.</description><identifier>ISSN: 0342-1791</identifier><identifier>EISSN: 1432-2021</identifier><identifier>DOI: 10.1007/s00269-012-0522-z</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Amorphization ; Bulk modulus ; Calcium ; Cations ; Compressibility ; Crystal structure ; Crystallography and Scattering Methods ; Crystals ; Curve fitting ; Density distribution ; Earth and Environmental Science ; Earth Sciences ; Equations of state ; Geochemistry ; High pressure ; Maximum entropy ; Maximum entropy method ; Mineral Resources ; Mineralogy ; Neutron diffraction ; Neutron scattering ; Neutrons ; Original Paper ; Phase transitions ; Pressure ; Thorium ; Unit cell ; X-ray diffraction</subject><ispartof>Physics and chemistry of minerals, 2012-09, Vol.39 (8), p.685-692</ispartof><rights>European Atomic Energy Community 2012</rights><rights>Physics and Chemistry of Minerals is a copyright of Springer, (2012). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c231z-bc0739ed9e9234dd76e693dc48495b90b234fc2b911fa37b6ae2a3b6a1e5240e3</citedby><cites>FETCH-LOGICAL-c231z-bc0739ed9e9234dd76e693dc48495b90b234fc2b911fa37b6ae2a3b6a1e5240e3</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/s00269-012-0522-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00269-012-0522-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Raison, Philippe E.</creatorcontrib><creatorcontrib>Heathman, Stephen</creatorcontrib><creatorcontrib>Wallez, Gilles</creatorcontrib><creatorcontrib>Zvoriste, Carmen E.</creatorcontrib><creatorcontrib>Bykov, Denis</creatorcontrib><creatorcontrib>Ménard, Gaël</creatorcontrib><creatorcontrib>Suard, Emmanuelle</creatorcontrib><creatorcontrib>Popa, Karin</creatorcontrib><creatorcontrib>Dacheux, Nicolas</creatorcontrib><creatorcontrib>Konings, Rudy J. M.</creatorcontrib><creatorcontrib>Caciuffo, Roberto</creatorcontrib><title>Structure and nuclear density distribution in the cheralite—CaTh(PO4)2: studies of its behaviour under high pressure (36 GPa)</title><title>Physics and chemistry of minerals</title><addtitle>Phys Chem Minerals</addtitle><description>The crystal structure of the cheralite—CaTh(PO
4
)
2
—has been revisited by neutron diffraction and its behaviour under high pressure investigated by X-ray diffraction up to 36 GPa. The neutron diffraction data at ambient pressure gave a more accurate determination of the Ca/Th cation position than previous XRD data, taking advantage that the neutron scattering lengths of calcium and thorium are of same order of magnitude. The nuclear density distribution was also determined using the maximum entropy method (MEM) confirming that the two cations are not located at the same position in the unit cell but are slightly displaced from one another along a specific direction in order to minimize the electrostatic repulsion with the surrounding phosphorus atoms. At high pressure, the compound did not show any phase transition or amorphization. From the evolution of the unit-cell volume as a function of the pressure, the zero-pressure bulk modulus B
0
and its pressure derivative B
0
′
have been determined by fitting the experimental compressibility curve to the Birch–Murnaghan equation of state. The results are B
0
= 140(2) GPa and B
0
′
= 4.4(4) GPa.</description><subject>Amorphization</subject><subject>Bulk modulus</subject><subject>Calcium</subject><subject>Cations</subject><subject>Compressibility</subject><subject>Crystal structure</subject><subject>Crystallography and Scattering Methods</subject><subject>Crystals</subject><subject>Curve fitting</subject><subject>Density distribution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Equations of state</subject><subject>Geochemistry</subject><subject>High pressure</subject><subject>Maximum entropy</subject><subject>Maximum entropy method</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Neutron diffraction</subject><subject>Neutron scattering</subject><subject>Neutrons</subject><subject>Original Paper</subject><subject>Phase transitions</subject><subject>Pressure</subject><subject>Thorium</subject><subject>Unit cell</subject><subject>X-ray diffraction</subject><issn>0342-1791</issn><issn>1432-2021</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kEtKBDEQhoMoOD4O4C7gRhetlUpPt3Engy8QFNR1SHeq7cjYPSZpYWblITyAZ_EonsQMI7hyVVD1P4qPsT0BRwKgPA4AWKgMBGYwRswWa2wkcokZAop1NgKZYyZKJTbZVgjPAOlYjkfs_T76oY6DJ246y7uhnpLx3FIXXJxz60L0rhqi6zvuOh5b4nVL3kxdpO_3j4l5aA_ubvNDPOUhDtZR4H3DXQy8ota8uX7wfOgsed66p5bPPIWwLDuQxdfn5Z053GEbjZkG2v2d2-zx4vxhcpXd3F5eT85ushqlWGRVDaVUZBUplLm1ZUGFkrbOT3I1rhRUadvUWCkhGiPLqjCERqYhaIw5kNxm-6vcme9fBwpRP6ffulSpEQuEEwlKJpVYqWrfh-Cp0TPvXoyfawF6CVqvQOsEWi9B60Xy4MoTkrZ7Iv-X_L_pB5AVgyA</recordid><startdate>201209</startdate><enddate>201209</enddate><creator>Raison, Philippe E.</creator><creator>Heathman, Stephen</creator><creator>Wallez, Gilles</creator><creator>Zvoriste, Carmen E.</creator><creator>Bykov, Denis</creator><creator>Ménard, Gaël</creator><creator>Suard, Emmanuelle</creator><creator>Popa, Karin</creator><creator>Dacheux, Nicolas</creator><creator>Konings, Rudy J. 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M. ; Caciuffo, Roberto</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c231z-bc0739ed9e9234dd76e693dc48495b90b234fc2b911fa37b6ae2a3b6a1e5240e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Amorphization</topic><topic>Bulk modulus</topic><topic>Calcium</topic><topic>Cations</topic><topic>Compressibility</topic><topic>Crystal structure</topic><topic>Crystallography and Scattering Methods</topic><topic>Crystals</topic><topic>Curve fitting</topic><topic>Density distribution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Equations of state</topic><topic>Geochemistry</topic><topic>High pressure</topic><topic>Maximum entropy</topic><topic>Maximum entropy method</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Neutron diffraction</topic><topic>Neutron scattering</topic><topic>Neutrons</topic><topic>Original Paper</topic><topic>Phase transitions</topic><topic>Pressure</topic><topic>Thorium</topic><topic>Unit cell</topic><topic>X-ray diffraction</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Raison, Philippe E.</creatorcontrib><creatorcontrib>Heathman, Stephen</creatorcontrib><creatorcontrib>Wallez, Gilles</creatorcontrib><creatorcontrib>Zvoriste, Carmen E.</creatorcontrib><creatorcontrib>Bykov, Denis</creatorcontrib><creatorcontrib>Ménard, Gaël</creatorcontrib><creatorcontrib>Suard, Emmanuelle</creatorcontrib><creatorcontrib>Popa, Karin</creatorcontrib><creatorcontrib>Dacheux, Nicolas</creatorcontrib><creatorcontrib>Konings, Rudy J. 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M.</au><au>Caciuffo, Roberto</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structure and nuclear density distribution in the cheralite—CaTh(PO4)2: studies of its behaviour under high pressure (36 GPa)</atitle><jtitle>Physics and chemistry of minerals</jtitle><stitle>Phys Chem Minerals</stitle><date>2012-09</date><risdate>2012</risdate><volume>39</volume><issue>8</issue><spage>685</spage><epage>692</epage><pages>685-692</pages><issn>0342-1791</issn><eissn>1432-2021</eissn><abstract>The crystal structure of the cheralite—CaTh(PO
4
)
2
—has been revisited by neutron diffraction and its behaviour under high pressure investigated by X-ray diffraction up to 36 GPa. The neutron diffraction data at ambient pressure gave a more accurate determination of the Ca/Th cation position than previous XRD data, taking advantage that the neutron scattering lengths of calcium and thorium are of same order of magnitude. The nuclear density distribution was also determined using the maximum entropy method (MEM) confirming that the two cations are not located at the same position in the unit cell but are slightly displaced from one another along a specific direction in order to minimize the electrostatic repulsion with the surrounding phosphorus atoms. At high pressure, the compound did not show any phase transition or amorphization. From the evolution of the unit-cell volume as a function of the pressure, the zero-pressure bulk modulus B
0
and its pressure derivative B
0
′
have been determined by fitting the experimental compressibility curve to the Birch–Murnaghan equation of state. The results are B
0
= 140(2) GPa and B
0
′
= 4.4(4) GPa.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s00269-012-0522-z</doi><tpages>8</tpages></addata></record> |
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| identifier | ISSN: 0342-1791 |
| ispartof | Physics and chemistry of minerals, 2012-09, Vol.39 (8), p.685-692 |
| issn | 0342-1791 1432-2021 |
| language | eng |
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| source | SpringerLink Journals |
| subjects | Amorphization Bulk modulus Calcium Cations Compressibility Crystal structure Crystallography and Scattering Methods Crystals Curve fitting Density distribution Earth and Environmental Science Earth Sciences Equations of state Geochemistry High pressure Maximum entropy Maximum entropy method Mineral Resources Mineralogy Neutron diffraction Neutron scattering Neutrons Original Paper Phase transitions Pressure Thorium Unit cell X-ray diffraction |
| title | Structure and nuclear density distribution in the cheralite—CaTh(PO4)2: studies of its behaviour under high pressure (36 GPa) |
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