Abstract
In situ X-ray diffraction and Raman spectroscopy of a synthetic whitlockite, Ca9Mg(PO3OH) (PO4)6, have been conducted at high pressures or high temperatures. The results show that whitlockite is stable up to ~15 GPa at ambient temperature and undergoes a thermally induced dehydrogenation to merrillite above 973 K at ambient pressure. The obtained pressure-volume data were fitted using a third-order Birch-Murnaghan equation of state, yielding an isothermal bulk modulus of K0 = 79(4) GPa with a pressure derivative of
Funding statement: This work was financially supported by the National Natural Science Foundation of China (Grant No. 42120104005), the International Partnership Program of Chinese Academy of Sciences (Grant No. 132852KYSB20200011), and Guizhou Provincial 2021 Science and Technology Subsidies (No. GZ2021SIG). The in-situ synchrotron X-ray diffraction measurements were carried out at the BL15U1 and BL14B1 beamlines of the Shanghai Synchrotron Radiation Facility (Proposal Nos. 2018-SSRF-PT-007075 and 2020-SSRF-PT-012550).
Acknowledgments
The authors thank Sergio Speziale for his editorial handling and helpful comments and suggestions and also appreciate Marina Martinez and Mario Tribaudino for their critical comments and suggestions.
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Articles in the same Issue
- Tetrahedral aluminum in tourmaline from a spinel-pargasite-metamorphosed mafic-ultramafic rock
- Lorenz number and transport properties of Fe: Implications to the thermal conductivity at Earth’s core-mantle boundary
- Structure and equation of state of Ti-bearing davemaoite: New insights into the chemical heterogeneity in the lower mantle
- Solfataric alteration at the South Sulfur Bank, Kilauea, Hawaii, as a mechanism for the formation of sulfates, phyllosilicates, and silica on Mars
- Plastic deformation and trace element mobility in sphalerite
- Crystallographic insights into monovalent thallium incorporation: Exploring hydropyrochlore structure for environmental remediation
- Distribution of REE between amphibole and pyroxenes in the lithospheric mantle: An assessment from the lattice strain model
- Elastic anomalies across the P21nm→Pnnm structural phase transition in δ-(Al,Fe)OOH
- Hyper-enrichment of heavy rare earth elements in highly evolved granites through multiple hydrothermal mobilizations
- In-situ zircon and cassiterite LA-ICP-MS geochronology and implications for granite-hosted Sn deposit models and exploration: Insights from the Cameroon Line
- Compressibility, thermal expansion, and Raman spectroscopy of synthetic whitlockite Ca9Mg(PO3OH)(PO4)6 at high pressures and high temperatures
- Experimental determination of tin partitioning between titanite, ilmenite, and granitic melts using improved capsule designs
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