A structural, infrared, and Mossbauer spectral study of rosemaryite, NaMnFe3+Al(PO4)3

  • Hatert F
  • Hermann R
  • Fransolet A
  • et al.
11Citations
Citations of this article
11Readers
Mendeley users who have this article in their library.

Abstract

Rosemaryite, ideally NaMnFe 3+ Al(PO 4 ) 3 , has been collected in the Buranga pegmatite, Rwanda. A single-crystal structure refinement was performed to R 1 = 4.01 %, in the P2 1 /n space group, with a = 12.001(2), b = 12.396(1), c = 6.329(1) Å, β = 114.48(1)°, Vol. = 856.9(2) Å 3 , Z = 4. The crystal structure and cation distributions are similar to those of ferrorosemaryite, NaFe 2+ Al(PO 4 ) 3 , and qingheiite, Na 2 MnMgAl(PO 4 ) 3 , but aluminium predominantly occurs in the M(2a) site, not in the M(2b) site as observed in ferrowyllieite, Na 2 Fe 2+ 2 Al(PO 4 ) 3 . The topologies of the X(1a) and X(1b) crystallographic sites are identical to those found in ferrorosemaryite, and correspond to a distorted octahedron and to a distorted cube, respectively. The [7+1]-coordinated X(2) site is a very distorted gable disphenoid, similar to the A(2)' site of the alluaudite structure. Mössbauer spectra have been obtained from 4.2 to 295 K, and fitted with a model including two Fe 3+ and two Fe 2+ doublets. The Fe 2+ component corresponding to 2/3 of the Fe 2+ spectral area and having a smaller quadrupole splitting of 2.63 mm/s at 15 K, is assigned to the Fe 2+ on the M(2a) site, and the Fe 2+ component with the larger quadrupole splitting of 3.17 mm/s at 15 K, is assigned to the Fe 2+ on the M(1) site. Fe 3+ is located only at the M(2a) and M(2b) sites, and the Fe 3+ component corresponding to 3/4 of the Fe 3+ and exhibiting the larger quadrupole spitting of 0.77 mm/s at 15 K, is most likely associated with Fe 3+ on the M(2b) site. The infrared spectrum of rosemaryite shows absorption bands at 3450 and 1624 cm -1 , bands that arise from the vibrational modes of H 2 O and confirm the presence of water in the channels of the wyllieite structure. A comparison of both the Mössbauer spectra and structural data of rosemaryite with those of other phosphates of the alluaudite and wyllieite groups, is also presented. © 2006 E. Schweizerbart'sche Verlagsbuchhandlung, D-70176 Stuttgart.

Cite

CITATION STYLE

APA

Hatert, F., Hermann, R. P., Fransolet, A.-M., Long, G. J., & Grandjean, F. (2006). A structural, infrared, and Mossbauer spectral study of rosemaryite, NaMnFe3+Al(PO4)3. European Journal of Mineralogy, 18(6), 775–785. https://doi.org/10.1127/0935-1221/2006/0018-0775

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free