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
Hauptverfasser: 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
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Sprache:eng
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Zusammenfassung: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.
ISSN:0342-1791
1432-2021
DOI:10.1007/s00269-012-0522-z