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American Mineralogist; April 2008; v. 93; no. 4; p. 698-701; DOI: 10.2138/am.2008.2827
© 2008 Mineralogical Society of America
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Letter

Crystal structure and Raman spectrum of hydroxyl-bästnasite-(Ce), CeCO3(OH)

Hexiong Yang1,*, Robert F. Dembowski1, Pamela G. Conrad2 and Robert T. Downs1

1 Department of Geosciences, University of Arizona, Tucson, Arizona 85721-0077, U.S.A.
2 Jet Propulsion Laboratory, MS-183-301, 4800 Oak Grove Drive, Pasadena, California 91109-8099, U.S.A.

Correspondence: * E-mail: hyang{at}u.arizona.edu

Hydroxyl-bästnasite-(Ce), ideally CeCO3(OH), had been regarded isostructural with bästnasite-(Ce), CeCO3F, the dominant member of the bästnasite family that produces ~70% of the world’s supply of rare-earth elements. Using single-crystal X-ray diffraction and Raman spectroscopy, our structural analysis on hydroxyl-bästnasite-(Ce) shows that the previous assumption is incorrect. The crystal structure of hydroxyl-bästnasite-(Ce) possesses PFormula symmetry with unit-cell parameters a = 12.4112(2), c = 9.8511(3) Å, and V = 1314.2(1) Å3, in contrast to the space group P Formula2c and a {approx} 7.10, c {approx} 9.76 A, and V {approx} 430 Å3 for bästnasite-(Ce). Moreover, there are 6, 3, and 5 symmetrically-distinct CO3 groups, Ce cations, and (OH/F) ions, respectively, in hydroxyl-bästnasite-(Ce), but 1, 1, and 2 in bästnasite-(Ce). The two structures, nevertheless, are similarly characterized by the layers of CO3 groups alternating with the Ce-(OH/F) layers along the c direction. The Raman spectrum of hydroxyl-bästnasite-(Ce) is dominated by three strong bands at 1080, 1087, and 1098 cm–1 in the CO3 symmetrical stretching region, along with at least four bands in the OH stretching region. Our study further suggests that natural hydroxyl-bästnasite-(Nd) is most likely isotypic with hydroxyl-bästnasite-(Ce), rather than with bästnasite-(Ce), as previously proposed.

Key Words: Bästnasite • hydroxyl-bästnasite-(Ce) • single-crystal X-ray diffraction • crystal structure • Raman spectra







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