Revealing the Incorporation of Cerium in Fluorapatite

Abstract

Fluorapatite (FAp, nominally Ca 5 (PO 4 ) 3 F) is the most common phosphate mineral at the Earth's surface and a main host for rare-earth elements (REE) in magmatic and hydrothermal ore deposits and in marine sediments. Our understanding of the enrichment process of REE in FAp rests upon two foundations: (1) being able to elucidate the thermodynamic driving force for their partitioning between Ca1 and Ca2 structural sites and (2) being able to determine how the substitution of REE(III) for Ca(II) is charge-compensated. A main unsolved question is the marked preference of the larger light REE (lanthanum → samarium) for the smaller Ca2 site. We used density functional theory (DFT) and high-energy-resolution fluorescence-detected extended X-ray absorption fine structure (HERFD-EXAFS) spectroscopy to gain detailed insight into the bonding energy, electronic structure, and short-range order of cerium (Ce) in natural magmatic/hydrothermal FAp. Results show that Ce(III) has a marked preference for a Ca2 site where the nearest five-valent phosphorus cation is replaced with a tetravalent silicon cation, thus balancing the charge excess of the Ce impurity locally. Atomic charge calculations show that the Ca2 site is more ionic than the Ca1 site and that the energetics of the site preference are linearly correlated to the ionization energy of the substituent. Cations with a low energy of ionization, such as Ce, preferably occupy the Ca2 site. Novel combination of HERFD-EXAFS spectroscopy and DFT appears to be the most straightforward and reliable way to assess the crystal chemistry of trace elements in compositionally complex natural materials and opens a previously unavailable avenue for mechanistic investigation of metal enrichment in ore deposits.

An Apatite-Group Praseodymium Carbonate Fluoroxybritholite: Hydrothermal Synthesis, Crystal Structure, and Implications for Natural and Synthetic Britholites

“…The mean M 1–O bond lengths of 2.573 Å are consistent with 2.523 Å in britholite-(Ce) . The M 2 (6h) site is predominately occupied by Pr with total occupancy of (Pr 0.85 Ca 0.15 ) 1.00 (Figure ), consistent with previous studies showing lanthanide preference for the M 2 site . The mean T 1–O bond lengths of 1.615 Å and its scattering factor are slightly less than those of full occupancy by Si atoms only.…”

“…75 The M 2 (6h) site is predominately occupied by Pr with total occupancy of (Pr 0.85 Ca 0.15 ) 1.00 ( Figure 6 ), consistent with previous studies showing lanthanide preference for the M 2 site. 76 The mean T 1–O bond lengths of 1.615 Å and its scattering factor are slightly less than those of full occupancy by Si atoms only. The thermal ellipsoid of X 1 site (see Supporting Information , Table S3 ) has elongation along c axis, a typical feature for fluorine-bearing apatite supergroup species.…”