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Electron paramagnetic resonance spectroscopic study of synthetic fluorapatite: Part III. Structural characterization of sub-ppm-level Gd and Mn in minerals at W-band frequency

¹ Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK S7N 5E2, Canada
² Department of Chemistry, University of Saskatchewan, Saskatoon, Saskachewan S7N 2C9, Canada
³ Illinois EPR Research Center, University of Illinois at Urbana-Champaign, Illinois 61801, U.S.A.
⁴ Canadian Light Source, University of Saskatchewan, Saskatoon, Saskachewan S7N 2C6, Canada

Correspondence: ^* E-mail: yuanming.pan{at}usask.ca

Room-temperature, single-crystal W-band (~94 GHz) electron paramagnetic resonance (EPR) spectra of a flux-grown fluorapatite (AP30-0) containing 0.8(1) ppm Gd and 0.9 ppm Mn disclose the presence of two even-isotope Gd³⁺ centers (electron spin number S = 7/2 and nuclear spin number I = 0) and a ⁵⁵Mn²⁺ center (S = I = 5/2). The relative abundance of the two Gd³⁺ centers (corresponding to recently established centers "a" and "b" containing Gd³⁺ ions at the Ca2 and Ca1 sites, respectively) in AP30-0 has been estimated to be 0.20, indicating that "a" in this sample arises from the presence of ~0.2 ppm Gd at the Ca2 site. In addition, high-resolution W-band spectra of this sample at ~120 and ~77 K disclose the ¹⁵⁵Gd and ¹⁵⁷Gd spectra of "a," in which these isotopes (I = 3/2) are only ~0.02 ppm in abundance. To the best of our knowledge, this is the first-ever demonstration of structural characterization of sub-ppm-level trace elements in minerals and their synthetic analogs. Moreover, the fact that the Gd³⁺ and ⁵⁵Mn²⁺ centers in AP30-0 are detected despite the multiplicity of lines arising from their complex fine structures, hyperfine structures, and magnetic-site splittings, suggests that the W-band EPR technique is potentially capable of characterizing trace elements with a single unpaired electron (S = 1/2) and zero nuclear spin (I = 0) at even lower concentrations.

The spin-Hamiltonian parameters of the ⁵⁵Mn²⁺ center, including matrices g, D, A, and P, and high-spin term of type S⁴, have been determined by optimization using the single-crystal W-band EPR spectra of a Gd-doped fluorapatite containing 3.0(4) ppm Mn. The principal-axis directions of D and the pseudo-symmetry axes calculated from the S⁴ parameters confirm that this center corresponds to occupancy of ⁵⁵Mn²⁺ ions at the Ca1 site. Also, the optimized parameters suggest that the Mn²⁺-substituted Ca1 site in the flux-grown fluorapatite has rhombic (i.e., triclinic) local symmetry [e.g., D/g_eß_e = 436.2(6) G, E/g_eß_e = 1.1(1) G], slightly different from the trigonal symmetry of the ideal Ca1 site.

This article has been cited by other articles:

				S. M. Nokhrin, Y. Pan, and M. J. Nilges Electron paramagnetic resonance spectroscopic study of carbonate-bearing fluorapatite: New defect centers and constraints on the incorporation of carbonate ions in apatites American Mineralogist, August 1, 2006; 91(8-9): 1425 - 1431. [Abstract] [Full Text] [PDF]