Skip to main content
Log in

Raman spectroscopy, vibrational analysis, and heating of buergerite tourmaline

  • Original Paper
  • Published:
Physics and Chemistry of Minerals Aims and scope Submit manuscript

Abstract

Polarized Raman spectra were collected for single crystal buergerite (NaFe3Al6(BO3)3Si6O18(O0.92(OH)0.08)3F) from room temperature to near 1,375°C. Vibrational assignments to features in the room temperature spectra were determined by lattice dynamics calculations, where internal BO3 motions dominate modes near 1,300 cm−1, internal SiO4 displacements dominate modes between 900 and 1,200 cm−1, while less localized displacements within the isolated Si6O18 ring mix with motions within Na, Fe, Al, F, and BO3 environments for fundamental modes below 780 cm−1. At elevated temperatures, most buergerite Raman features broaden and shift to lower frequencies up to 900°C. Above this temperature, the lattice mode peaks evolve into broad bands, while OH stretch modes near 3,550 cm−1 disappear. According to Raman spectroscopy, X-ray diffraction, differential thermal analysis, and scanning electron microscopy, buergerite undergoes a complex transition that starts near 700°C and extends over a 310°C interval, where initially, Al and Fe probably become disordered within the Y- and Z-sites, and most F and all OH are later liberated. A reversible crystal-to-amorphous transition is seen by Raman for buergerite fragments heated as high as 930°C. Buergerite becomes permanently altered when heated to temperatures greater than 930°C; after cooling to room temperature, these altered fragments are comprised of mullite and Fe-oxide crystals suspended in an amorphous borosilicate matrix.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6

Similar content being viewed by others

References

  • Afonina GG, Bogdanova LA, Makagon VM (1993) Changes of Y and Z octahedra of the tourmaline structure under its thermal working from X-ray powder patterns. Zapiski Vserossiyskogo Miner Obshchestva 122/6:89–98

    Google Scholar 

  • Alvarez MA, Coy-Yll R (1977) Raman spectra of tourmaline. Spectrochim Acta 34A:899–908

    Google Scholar 

  • Dowty E (1987) Vibrational interactions of tetrahedra in silicate glasses and crystals. Phys Chem Miner 14:122–138

    Article  Google Scholar 

  • Dowty E (2007) Vibratz2.0 software details available at http://www.shapesoftware.com

  • Dyar MD, Taylor ME, Lutz TM, Francis CA, Guidotti CV, Wise M (1998) Inclusive chemical characterization of tourmaline: Mössbauer study of Fe valence and site occupancy. Am Miner 83:848–864

    Google Scholar 

  • Ertl A, Hughes JM (2002) The crystal structure of an aluminum-rich schörl overgrown by boron-rich olenite from Koralpe, Styria, Austria. Mineral Petrol 75:69–78

    Article  Google Scholar 

  • Ertl A, Hughes JM, Brandstatter F, Dyar MD, Prasad PSR (2003) Disordered Mg-bearing olenite from a granitic pegmatite at Goslarn, Austria: a chemical, structural, and infrared spectroscopic study. Can Mineral 41:1363–1370

    Article  Google Scholar 

  • Fateley WG, Dollish FR, McDevitt NT, Bentley FF (1972) Infrared and Raman selection rules for molecular and lattice vibrations: the correlation method. Wiley, New York

    Google Scholar 

  • Gasharova B, Mihailova B, Konstantinov L (1997) Raman spectra on various types of tourmaline. Eur J Miner 9:935–940

    Google Scholar 

  • Goncharov AF, Struzhkin VV (2003) Raman spectroscopy of metals, high-temperature superconductors, and related materials under high pressure. J Raman Spectrosc 34:538–548

    Article  Google Scholar 

  • Hawthorne FC, Henry DJ (1999) Classification of the minerals of the tourmaline group. Eur J Miner 11:201–215

    Google Scholar 

  • Henry DJ, Dutrow BL (1996) Metamorphic tourmaline and its petrologic applications. In: Grew ES, Anovitz LM (eds) Boron: mineralogy, petrology, and geochemistry. Reviews in mineralogy, vol 33, chap 10. Mineralogical Society of America, Washington, DC, pp 503–557

  • Kim CC, Bell MI, McKeown DA (1993) Vibrational analysis of benitoite (BaTiSi3O9) and the Si3O9 ring. Phys Rev B 47:7869–7877

    Article  Google Scholar 

  • Krosse S (1995) Hochdrucksynthese, Stabilitat und Eigenschaften der Borsilikate Dravit und Kornerupin sowie Darstellung und Stabilitatsverhalten eines neuen Mg-Al-borates. Unpublished Doctor’s Thesis, Ruhr-Universitat, Bochum

  • McKeown DA, Bell MI, Kim CC (1993) Raman spectroscopy of silicate rings: benitoite and the 3-membered ring. Phys Rev B 48:16357–16365

    Article  Google Scholar 

  • McKeown DA, Bell MI, Etz ES (1999a) Vibrational analysis of the trioctahedral mica phlogopite. Am Min 84:970–976

    Google Scholar 

  • McKeown DA, Bell MI, Etz ES (1999b) Vibrational analysis of muscovite: a dioctahedral mica. Am Min 84:1041–1048

    Google Scholar 

  • Mihailova B, Gasharova B, Konstantinov L (1996) Influence of non-tetrahedral cations in Si–O vibrations in complex silicates. J Raman Spectrosc 27:829–833

    Article  Google Scholar 

  • Nasdala L, Banerjee A, Hager T, Hofmeister W (2001) Laser Raman micro-spectroscopy in mineralogical research. Microsc Anal 15:7–9

    Google Scholar 

  • Pieczka A, Kraczka J (2004) Oxidized tourmalines—a combined chemical, XRD, and Mössbauer study. Eur J Miner 16:309–321

    Article  Google Scholar 

  • Slack JF (1996) Tourmaline associations with hydrothermal ore deposits. In: Grew ES, Anovitz LM (eds) Boron: mineralogy, petrology, and geochemistry. Reviews in mineralogy, vol 33, chap 11. Mineralogical Society of America, Washington, DC, pp 559–643

  • Smith DC, Gendron F (1998) Archaeometric application of the Raman microprobe to the non-destructive identification of two pre-Columbian ceremonial polished greenstone axe-heads from Meso-America. J Raman Spec 28:731–738

    Article  Google Scholar 

  • Tippe A, Hamilton WC (1971) A neutron-diffraction study of the ferric tourmaline, buergerite. Am Min 56:101–113

    Google Scholar 

  • Thomas R (2000) Determination of water contents in gramite melt inclusions by confocal laser Raman microprobe spectroscopy. Am Min 85:868–872

    Google Scholar 

  • Thomas R, Kamenetsky VS, Davidson P (2006) Laser Raman spectroscopic measurements of water in unexposed glass inclusions. Am Min 91:467–470

    Article  Google Scholar 

  • Werding G, Schreyer W (1996) Experimental studies on borosilicates and selected borates. In: Grew ES, Anovitz LM (eds) Boron: mineralogy, petrology, and geochemistry. Reviews in mineralogy, vol 33, chap 3. Mineralogical Society of America, Washington, DC, pp 149–154

  • Zotov N, Keppler H (1998) The influence of water on the structure of hydrous sodium tetrasilicate glass. Am Min 83:823–834

    Google Scholar 

Download references

Acknowledgments

The author thanks A. Piezcka and L. Nasdala for their constructive reviews of this manuscript. The author also thanks J. Post and P. Pohwat (Mineral Sciences Department, Smithsonian Institution) for providing the buergerite crystals. SEM analyses performed by Fr. A. Buechele (Vitreous State Laboratory, VSL) and the DTA experiments performed by C. Viragh (VSL) are also appreciated.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to David A. McKeown.

Rights and permissions

Reprints and permissions

About this article

Cite this article

McKeown, D.A. Raman spectroscopy, vibrational analysis, and heating of buergerite tourmaline. Phys Chem Minerals 35, 259–270 (2008). https://doi.org/10.1007/s00269-008-0219-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00269-008-0219-5

Keywords

Navigation