journal article·2010-02Open access

Temperature dependence of the OH-stretching frequencies in topaz-OH

Anke Watenphul, Bernd Wunder

Physics and Chemistry of Minerals· Volume 37· Issue 2

Abstract

Hydrogen bonding in topaz-OH, Al2SiO4(OH)2, was investigated by IR spectroscopic analysis of the temperature dependence of the OH-stretching frequencies. Low-temperature spectra ranging from −196 to −160°C prove the existence of four non-equivalent H-positions in the crystal structure from the occurrence of four different OH-bands. With increasing temperature, these bands merge first, above −160°C, into two OH-bands and then above 400°C into one asymmetric broad band. Shifting of the OH-bands is caused by thermally induced hydrogen order–disorder. Low temperature fixes the protons in their positions; increasing temperature induces proton movement and allows switching between the different positions. Autocorrelation analysis of the IR spectra reveals two phase transitions, one at about −155°C from P1 to Pbn2 1 characterized as static–dynamic change and the second at about 380°C from Pbn2 1 to Pbnm caused by disordering of the protons. The increasing symmetry with temperature is due to advanced proton movement and dynamical averages over the proton distribution densities.
Source: openaire · Quality: candidate unverified · Source record ↗

Research context

OpenAlex topics: Mineralogy and Gemology Studies · Geological and Geochemical Analysis · Geology and Paleoclimatology Research

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

References (26)

Show source-provided references
1. Abbott RN Jr (1990) Topaz: energy calculations bearing on the location of hydrogen. Can Mineral 28:827–833
2. Barton MD (1982) The thermodynamic properties of topaz solid solution and some petrological applications. Am Mineral 67:956–974
3. Chen J, Lager GA, Kunz M et al (2005) A Rietveld refinement using neutron powder diffraction data of a fully deuterated topaz, Al2SiO4(OD)2. Acta Crystallogr E. doi: 10.1107/S160053680503481110.1107/S1600536805034811 ↗
4. Churakov SV, Wunder B (2004) Ab initio calculations of the proton location in topaz-OH, Al2SiO4(OH)2. Phys Chem Miner 31:131–141. doi: 10.1007/s00269-003-0365-810.1007/s00269-003-0365-8 ↗
5. Domanik KJ, Holloway JR (1996) The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: implications for deeply subducted sediments. Geochim Cosmochim Acta 60(21):4133–4415. doi: 10.1016/S0016-7037(96)00241-410.1016/S0016-7037(96)00241-4 ↗
6. Fei Y (1995) Thermal expansion. In: Mineral physics and crystallography a handbook of physical constants. AGU Ref Shelf 2:29–43
7. Griffiths PR, de Haseth JA (1986) Fourier transform infrared spectroscopy. Wiley, New York
8. Komatsu K, Kagi H, Okada T et al (2005) Pressure dependence of the OH-stretching mode in F-rich natural topaz and topaz-OH. Am Mineral 90:266–270. doi: 10.2138/am.2005.165210.2138/am.2005.1652 ↗
9. Komatsu K, Kagi H, Marshall WG et al (2008) Pressure dependence of the hydrogen-bond geometry in topaz-OD from neutron powder diffraction. Am Mineral 93:217–227. doi: 10.2138/am.2008.248310.2138/am.2008.2483 ↗
10. Larson AC, von Dreele RB (2004) Generalized structure analysis system. Los Alamos Nat Lab Rep LAUR 9:6–748
11. Libowitzky E, Beran A (2004) IR spectroscopic characterisation of hydrous species in minerals. In: Beran A, Libowitzky E (eds) Spectroscopic methods in mineralogy, EMU notes in mineralogy, vol 6, pp 227–27910.1180/EMU-notes.6.6 ↗
12. Libowitzky E, Rossman GR (1997) IR absorption calibration for water in minerals. Am Mineral 82:1111–111510.2138/am-1997-11-1208 ↗
13. Mertz L (1965) Transformation in optics. Wiley, New York
14. Northrup PA, Leinenweber K, Parise JB (1994) The location of H in the high-pressure synthetic Al2SiO4(OH)2 topaz analogue. Am Mineral 79:401–404
15. Ono S (1998) Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions: implications for water transport in subduction zones. J Geophys Res 103(B8):18253–18267. doi: 10.1029/98JB0135110.1029/98JB01351 ↗
16. Ono S (1999) High temperature stability limit of phase egg, AlSiO3(OH). Contrib Mineral Petrol 137:83–89. doi: 10.1007/s00410005058310.1007/s004100050583 ↗
17. Ribbe PH (1982) Topaz. In: Ribbe PH (ed) Orthosilicates. Reviews in Mineralogy, 2rd edn, pp 215–23010.1515/9781501508622-014 ↗
18. Salje E, Carpenter MA, Malcherek T et al (2000) Autocorrelation analysis of infrared spectra from minerals. Eur J Mineral 12:503–51910.1127/0935-1221/2000/0012-0503 ↗
19. Schmidt MW (1995) Lawsonite: upper pressure stability and formation of higher density hydrous phases. Am Mineral 80:1286–129210.2138/am-1995-11-1218 ↗
20. Schreyer W (1995) Ultradeep metamorphic rocks: retrospective viewpoint. J Geophys Res 100(B5):8353–8366. doi: 10.1029/94JB0291210.1029/94JB02912 ↗
21. Theye T (1988) Aufsteigende Hochdruckmetamorphose in Sedimenten der Phyllit-Quarzit-Einheit Kretas und des Peloponnes. Ph.D. thesis, University of Braunschweig
22. Watenphul A, Wunder B, Heinrich W (2009) High-pressure ammonium-bearing silicates: implications for nitrogen and hydrogen storage in the Earth’s mantle. Am Mineral 94:283–29210.2138/am.2009.2995 ↗
23. Wunder B, Rubie DC, Ross CDII et al (1993) Synthesis, stability, and properties of Al2SiO4(OH)2: a fully hydrated analogue of topaz. Am Mineral 78:285–297
24. Wunder B, Andrut M, Wirth R (1999) High-pressure synthesis and properties of OH-rich topaz. Eur J Mineral 11:803–81310.1127/ejm/11/5/0803 ↗
25. Xue X, Kanzaki M, Fukui H et al (2006) Cation order and hydrogen bonding of high-pressure phases in the Al3O3–SiO2–H2O system: an NMR and Raman study. Am Mineral 91:850–861. doi: 10.2138/am.2006.206410.2138/am.2006.2064 ↗
26. Zhang RY, Liou JG, Shu JF (2002) Hydroxyl-rich topaz in high-pressure and ultrahigh-pressure kyanite quartzites, with retrograde woodhousite, from the Sulu terrane, eastern China. Am Mineral 87:445–45310.2138/am-2002-0408 ↗