Skip to main content

Advertisement

Log in

Uncertainties on elastic parameters and occupancy factors: how do they affect the accuracy of the calculated Gibbs energy of minerals at (P,T) conditions? The case of 3T- versus 2M 1-phengite

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

Abstract

The present paper reports a study about how the uncertainties on some fundamental thermodynamic and structural quantities (formation enthalpy, specific heat, thermo-elastic properties, occupancy factors) propagate and affect the Gibbs energy calculated at given pressure and temperature conditions [G(P,T)] for mineral phases. A particular attention is paid to the role played by the uncertainties on the bulk modulus, its first derivative versus pressure, molar volume at a reference condition, i.e. V 0, and occupancy factors. The calculations in question are carried out for three phases: 2M 1-phengite, olivine and MgAl-spinel, in order to provide coverage for thermo-elastic parameters values common in a variety of natural processes. Above a few GPa, the uncertainty due to the deformation energy, i.e. σ[ΔG deform], and dependent on the parameters governing the equation of state, grows the dominant contribution to the total uncertainty on G(P,T), i.e. σ[G(P,T)]. σ[ΔG deform] is very sensitive to V 0, but the comparatively small σ(V 0)/V 0 value makes the V 0-contribution to σ[ΔG deform] less relevant than those due to the elastic parameters. The stability curve of 3T- versus 2M 1-phengite as a function of pressure (Curetti et al. in Phys Chem Mineral 32:670–678, 2006) is here revised in the light of the uncertainty on G(P,T): an improvement of accuracy such as to reduce the uncertainty on bulk modulus and its first derivative versus pressure by a 0.05 factor is, in principle, required to guarantee a fully unambiguous description of the relative stability between these two phases.

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

  • Angel R (2000) Equations of state. In: Hazel RM, Downs RT (eds) High-temperature and high-pressure crystal chemistry. Mineralogical Society of America Geochemical Society, Reviews in Mineralogy and Geochemistry, vol 41, pp 35–59

  • Askarpour V, Manghnani MH, Fassbender S, Yoneda A (1993) Elasticità of single-crystal MgAl2O4 spinel up to 1,273 K by Brillouin spectroscopy. Phys Chem Miner 19:511–519

    Article  Google Scholar 

  • Bass JD, Liebermann RC, Weidner DJ, Finch SJ (1981) Elastic properties from acoustic and volume compression experiments. Phys Earth Planet Int 25:140–158

    Article  Google Scholar 

  • Birch F (1986) Equation of state and thermodynamic parameters of NaCl to 300 kbar in the high-temperature domain. J Geophys Res 91:4949–4954

    Article  Google Scholar 

  • Carpenter MA, Powell R, Salje EKH (1994) Thermodynamics of nonconvergent cation ordering in minerals: I. An alternative approach. Am Mineral 79:1053–1067

    Google Scholar 

  • Catti C, Pavese A, Price GD (1993) Thermodynamic properties of CaCO3 calcite and aragonite: a quasi-harmonic calculation. Phys Chem Miner 19:472–479

    Article  Google Scholar 

  • Connolly JAD (1990) Multivariable phase diagrams: an algorithm based on generalized thermodynamics. Am J Sci 290:666–718

    Article  Google Scholar 

  • Curetti N, Levy D, Pavese A, Ivaldi G (2006) Elastic properties and stability of coexisting 3T and 2M1 phengite polytypes. Phys Chem Mineral 32:670–678

    Article  Google Scholar 

  • Duffy TS, Wang Y (1998) Pressure–volume–temperature equations of state. In: Hemley RJ (ed) Ultrahigh-pressure mineralogy. Mineralogical Society of America, Reviews in Mineralogy, vol 37, pp 425–458

  • Ferraris G, Ivaldi G (2002) Structural features of micas. In: Mottana A, Sassi FP, Thompson JB, Guggenheim S (eds) Micas: crystal chemistry and metamorphic petrology. Accademia Nazionale dei Lincei, Geochemical Society, and Mineralogical Society of America, Reviews in Mineralogy and Geochemistry, vol 46, pp 117–153

  • Ferraris G, Ivaldi G, Nespolo M, Takeda H (1995) On the stability of dioctahedral micas. Terra Abstr, Suppl N.1 Terra Nova 7:289

  • Guidotti CV, Sassi FP (2002) Constraints on studies of metamorphic K–Na white micas. In: Mottana A, Sassi FP, Thompson JB Jr, Guggenheim S (eds) Micas: crystal chemistry and metamorphic petrology. Accademia Nazionale dei Lincei, Geochemical Society, and Mineralogical Society of America, Reviews in Mineralogy and Geochemistry, vol 46, pp 413–448

  • Guidotti CV (1984) Micas in metamorphic rocks. In: Bailey SW (ed) Micas. Mineralogical Society of America, Reviews in Mineralogy 13:357–467

  • Hazel RM (1976) Effect of temperature and pressure on the crystal structure of forsterite. Am Mineral 61:1280–1293

    Google Scholar 

  • Holland TJB, Powell R (1998) An internally consistent data set for phases of petrological interest. J Metamorph Geol 16:309–343

    Article  Google Scholar 

  • Levy D, Pavese A, Hanfland M (2003) Synthetic MgAl2O4 (spinel) at high-pressure conditions (0.0001–30 GPa): an X-ray powder diffraction by synchrotron radiation. Am Mineral 88:93–98

    Google Scholar 

  • Levy D, Diella V, Dapiaggi M, Sani A, Gemmi M, Pavese A (2004) Equation of state, structural behavior and phase diagram of synthetic MgFe2O4, as a function of pressure and temperature. Phys Chem Miner 31:122–129

    Article  Google Scholar 

  • Levy D, Diella V, Pavese A, Dapiaggi M, Sani A (2005) PV equation of state, thermal expansion and PT stability of synthetic ZnCr2O4 spinel. Am Mineral 90:1157–1162

    Article  Google Scholar 

  • Meng Y, Weidner DJ, Gwanmesia GD, Liebermann RC, Vaughan MT, Wang Y, Leinenweber K, Pacalo RE, Yeganeh-Haeri A, Zhao Y (1993) In situ high PT X ray diffraction studies on three polymorphs (alpha, beta, gamma) of Mg2SiO4. J Geophys Res B Solid Earth Planets 98:22199–22207

    Google Scholar 

  • Nespolo M, Duroviç S (2002) Crystallographic basis of polytypism and twinning in micas. In: Mottana A, Sassi FP, Thompson JB, Guggenheim S (eds) Micas: crystal chemistry and metamorphic petrology. Accademia Nazionale dei Lincei, Geochemical Society, and Mineralogical Society of America, Reviews in Mineralogy and Geochemistry, vol 46, pp 155–279

  • O’Neill HStC, Navtrosky A (1983) Simple spinels: crystallographic parameters, cation radii, lattice energies and cation distributions. Am Mineral 68:181–194

    Google Scholar 

  • O’Neill HStC, Navtrosky A (1984) Cation distribution and thermodynamic properties of binary spinel solid solutions. Am Mineral 69:733–753

    Google Scholar 

  • Pavese A (2002) Pressure volume temperature equations of state: a comparative study based on numerical simulations. Phys Chem Miner 29:43–51

    Article  Google Scholar 

  • Pavese A, Ferraris G, Prencipe M, Ibberson R (1997): Cation site ordering in phengite 3T from the Dora-Maira massif (western Alps): a variable-temperature neutron powder diffraction study. Eur J Mineral 9:1183–1190

    Google Scholar 

  • Pavese A, Ferraris G, Pischedda V, Ibberson R (1999a) Tetrahedral order in phengite 2M1 upon heating, from powder neutron diffraction, and thermodynamic consequences. Eur J Mineral 11:309–320

    Google Scholar 

  • Pavese A, Ferraris G, Pischedda V, Mezouar M (1999b) Synchrotron powder diffraction study of phengite 3T from the Dora-Maira massif: PVT equation of state and petrological consequences. Phys Chem Miner 26:460–467

    Article  Google Scholar 

  • Pavese A, Ferraris G, Pischedda V, Radaelli P (2000a) Further study of the cation ordering in phengite 3T by neutron powder diffraction. Mineral Mag, 64:11–18

    Article  Google Scholar 

  • Pavese A, Artioli G, Hoser A (2000b) Mg–Al synthetic spinels: cation and vacancy distribution as a function of temperature, from neutron powder diffraction. Z Kristallogr 215:406–412

    Article  Google Scholar 

  • Pavese A, Ferraris G, Pischedda V, Fauth R (2001) M1-site occupancy in 3T and 2M1 phengites by low temperature neutron powder diffraction: reality or artefact? Eur J Mineral 13:1071–1078

    Article  Google Scholar 

  • Peterson RC, Lager GA, Hitterman RL (1991) A time-of-flight neutron powder diffraction study of MgAl2O4 at temperatures up to 1,273 K. Am Mineral 76:1455–1458

    Google Scholar 

  • Redfern SAT, Harrison RJ, O’Neill HStC, Wood DRR (1999) Thermodynamics and kinetics of cation ordering in MgAl2O4 spinel up to 1,600°C from in situ neutron diffraction. Am Mineral 84:299–310

    Google Scholar 

  • Redfern SAT, Artioli G, Rinaldi R, Henderson CMB, Knight KS, Wood BJ (2000) Octahedral cation ordering in olivine at high temperature. II: an in situ neutron powder diffraction study on synthetic MgFeSiO4 (Fa50). Phys Chem Miner 27:630–537

    Article  Google Scholar 

  • Sassi FP, Guidotti CV, Rieder M, De Pieri R (1994) On the occurence of metamorphic 2M1 pengites: some thoughts on polytypism and crystallization condition of 3T phengites. Eur J Mineral 6:151–160

    Google Scholar 

  • Shim SH, Duffy TS (2000) Constraints on the PVT equation of state of MgSiO3 perovskite. Am Mineral 85:354–363

    Google Scholar 

  • Smyth JR, Jacobsen SD, Swope RJ, Angel RJ, Arlt T, Domanik K, Holloway JR (2000) Crystal structures and compressibilities of synthetic 2M1 and 3T phengite micas. Eur J Mineral 12:955–963

    Google Scholar 

  • Stixrude L, Lithgow-Bertelloni C (2005) Thermodynamics of mantle minerals—I physical properties. Geophys J Int 162:610–632

    Article  Google Scholar 

  • Vieillard Ph (1995) How do uncertainties of the structure refinements influence the accuracy of the prediction of enthalpy of formation? Examples on muscovite and natrolite. Phys Chem Miner 22:428–436

    Article  Google Scholar 

  • Wei C, Powell R (2004) Calculated phase relations in high-pressure metapelites in the system NKFMASH (Na2O–KO2–FeO–MgO–Al2O3–SiO2–H2O). J Petrol 45:183–202

    Article  Google Scholar 

Download references

Acknowledgments

Italian Ministry for University and Research (M.U.R.S.T) and Italian National Research Council (C.N.R) are kindly acknowledged for contributing to fund the investigations in question. The authors are grateful to the reviewers for comments to improve the quality of the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Alessandro Pavese.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pavese, A., Diella, V. Uncertainties on elastic parameters and occupancy factors: how do they affect the accuracy of the calculated Gibbs energy of minerals at (P,T) conditions? The case of 3T- versus 2M 1-phengite. Phys Chem Minerals 34, 637–645 (2007). https://doi.org/10.1007/s00269-007-0179-1

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00269-007-0179-1

Keywords

Navigation