Skip to main content
Log in

Annite stability revised. 1. Hydrogen-sensor data for the reaction annite = sanidine + magnetite + H2

  • Published:
Contributions to Mineralogy and Petrology Aims and scope Submit manuscript

Abstract

In P - T - logfO2 space, the stability of annite (ideally KFe 2+3 (OH)2AlSi3O10) at high fO2 (low fH2) is limited by the reaction: annite = sanidine + magnetite + H2. Using the hydrogen-sensor technique, the equilibrium fH2 of this reaction was measured between 500 and 800° C at 2.8 kbar in 50° C intervals. Microbrobe analyses of the reacted annite+sanidine+magnetite mixtures show that tetrahedral positions of annite have a lower Si/Al ratio than the ideal value of 3/1. Silicon decreases from ∼2.9 per formula unit at low temperatures to ∼2.76 at high temperatures. As determined by Mössbauer spectroscopy in three experimental runs, the Fe3+ content of annite in the equilibrium assemblage is 11%±3. A least squares fit to the hydrogensensor data gives ΔH 0R = 50.269 ± 3.987 kJ and ΔS 0R = 83.01 ± 4.35 J/K for equilibrium (1). The hydrogene-sensor data are consistent with temperature half brackets determined in the classical way along the nickel-nickel oxide (NNO) and quartz-fayalite-magnetite (QFM) buffers with a mixture of annite+sanidine+magnetite for control. Compared to published oxygen buffer reversals, agreement is only found at high temperature and possible reasons for that discrepancy are discussed. The resulting slope of equilibrium (1) in logfO2T dimensions is considerably steeper than previously determined and between 400 and 800°C only intersects with the QFM buffer curve. Based on the hydrogen-sensor data and on the thermodynamic dataset of Berman (1988, and TWEEQ data base) for sanidine, magnetite and H2, the deduced standard-state properties of annite are: H 0f =-5127.376±5.279 kJ and S 0=422.84±5.29 J/(mol K). From the recently published unit cell refinements of annites and their Fe3+ contents, determined by Mössbauer spectroscopy (Redhammer et al. 1993), the molar volume of pure annite was constrained as 15.568±0.030 J/bar. A revised stability field for annite is presented, calculated between 400 and 800°C.

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.

Similar content being viewed by others

References

  • Appleman DE, Evans HT (1973) Indexing and least-squares refinements of powder diffraction data. US Geol Surv Comput Contrib 20

  • Berman RG (1988) Internally consistent thermodynamic data for stoichiometric minerals in the system Na2O−K2O−CaO−MgO−FeO−Fe2O3−Al2O3−SiO2−TiO2−H2O−CO2. J Petrol 29:445–522.

    Google Scholar 

  • Berman RG (1990) Mixing properties of Ca−Mg−Fe−Mn garnets. Am Mineral 75:328–344

    Google Scholar 

  • Berman RG (1991) Thermobarometry using multi-equilibrium calculations: a new technique, with petrological applications. Can Mineral 29:833–855

    Google Scholar 

  • Chou IM (1987a) Oxyten buffer and hydrogen-sensor techniques at elevated pressures and temperatures. In: Ulmer GC, Barnes HL (eds) Hydrothermal experimental techniques. John Wiley and Sons, New York, pp. 61–100

    Google Scholar 

  • Chou IM (1987b) Calibration of the graphite-methane buffer using fH2 sensors at 2 kbar pressure. Am Mineral 72:76–81

    Google Scholar 

  • Chou IM, Eugster HP (1976) A sensor for hydrogen fugacities at elevated P and T and applications. Trans Am Geophys Union 57:340

    Google Scholar 

  • Eugster HP (1957) Heterogeneous reactions involving oxidation and reduction at high pressures and temperatures. J Chem Phys 26:1160

    Google Scholar 

  • Eugster HP (1959) Reduction and oxidation in metamorphism. In: Abelson PH (ed) Researches in geochemistry. John Wiley and Sons, New York, pp 397–426

    Google Scholar 

  • Eugster HP, Wones DR (1962) Stability relations of the ferruginous biotite, annite, J Petrol 3:82–125

    Google Scholar 

  • Ferrow E, Annersten H (1984) Ferric iron in trioctahedral micas. Univ Uppsala UUDMP Res Rep 39

  • Ferry JM, Spear F (1978) Experimental calibration of the partitioning of Fe and Mg between biotite and garnet. Contrib Mineral Petrol 66:113–117

    Google Scholar 

  • Fonarev VI, Konilov AN (1986) Experimental study of Fe−Mg distribution between biotite and orthopyroxene. Contrib Mineral Petrol 93:227–235

    Google Scholar 

  • Frantz JD, Marshall WL (1984) Electrical conductances and ionization constants of salts, acids, and bases in supercritical aqueous fluids. I. Hydrochloric acid from 100 to 700° C and at pressures to 4000 bars. Am J Sci 284:651–667

    Google Scholar 

  • Grevel KD, Chatterjee ND (1992) A modified Redlich-Kwong equation of state for H2−H2O fluid mixtures at high pressures and at temperatures above 400° C. Eur J Mineral 4:1303–1310

    Google Scholar 

  • Hamilton DL, Henderson CMB (1968) The preparation of silicate compositions by a gelling method. Miner Mag 36: 832–838

    Google Scholar 

  • Hazen RM, Wones DR (1972) The effect of cation substitutions on the physical properties of trioctahedral micas. Am Mineral 57:103–129

    Google Scholar 

  • Hewitt DA, Wones DR (1975) Physical properties of some synthetic Fe−Mg−Al trioctahedral biotites. Am Mineral 60:854–862

    Google Scholar 

  • Hewitt DA, Wones DR 1981 The annite-sanidine-magnetite equilibrium (abstract) GAC-MAC J Annu Meet Calgary Abstr 6:A–66

    Google Scholar 

  • Hewitt DA, Wones DR (1984) Experimental phase relations of the micas. In: Bailey SW (ed) Micas. (Reviews in mineralogy, vol 13) Book Crafters, Chelsea, Michigan, pp 201–256

    Google Scholar 

  • Holland TJ, Powell R (1985) An internally consistent thermodynamic dataset with uncertainties and correlations. 2. Data and results. J metamorphic Geol 3:343–370

    Google Scholar 

  • Holland TJB, Powell R (1990) An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K2O−Na2O−CaO−MgO−MnO−FeO−Fe2O3−Al2O3−TiO2−SiO2−C−H2−O2. J metamorphic Geol 8:89–124

    Google Scholar 

  • Kohn MJ, Spear FS (1991) Error propagation for barometers. 2. Application to rocks. Am Mineral 76:138–147

    Google Scholar 

  • McMullin DWA, Berman G, Greenwood HJ (1991) Calibration of the SGAM thermobarometer for pelitic rocks using data from phase-equilibrium experiments and natural assemblages. Can Mineral 29:889–908

    Google Scholar 

  • Moecher DP, Chou IM (1990) Experimental investigation of andradite and hedenbergite equilibria employing the hydrogensensor technique, with revised estimates of Δf G Om, 298 andradite and hedenbergite. Am Mineral 75:1327–1341

    Google Scholar 

  • O'Neill HStC (1987a) Free energies of formation of NiO, CoO, Ni2SiO4, and Co2SiO4. Am Mineral 72:280–291

    Google Scholar 

  • O'Neill HStC (1987b) Quartz-fayalite-iron and quartz-fayalite-magnetite equilibria and the free energy of formation of fayalite (Fe2SiO4) and magnetite (Fe3O4). An Mineral 72: 67–75

    Google Scholar 

  • O'Neill HStC (1988) Systems Fe−O and Cu−O: thermodynamic data for the equilibria Fe−“FeO”, Fe−Fe3O4, “FeO”−Fe3O4, Fe3O4−Fe2O3, Cu−Cu2O, and Cu2O−CuO from emf measurements. Am Mineral 73:470–486

    Google Scholar 

  • Partin E, Hewitt DA, Wones DR (1983) Quantification of ferric iron in biotite (abstract). Geol Soc Am Abstr Program 15:659

    Google Scholar 

  • Powell R (1985) Geothermometry and geobarometry: a discussion. J Geol Soc London 142:29–38

    Google Scholar 

  • Powell R, Holland TJB (1985) An internally consistent thermodynamic dataset with uncertainties and correlations. 1. Methods and a worked example. J metamorphic Geol 3:327–342

    Google Scholar 

  • Redhammer GJ, Beran A, Dachs E, Amthauer G (1993) A Mössbauer and X-ray diffraction study of annites synthesized at different oxygen fugacities and crystal chemical implications. Phys Chem Miner 20:382–394

    Google Scholar 

  • Robie RA, Hemingway BS, Fisher JR (1978) Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (105 pascals) pressure and at higher temperatures. US Geol Surv Bull 1452

  • Rutherford MJ (1969) An experimental determination of iron biotite-alkali feldspar equilibria. J Petrol 10:381–408

    Google Scholar 

  • Wolfram Research Inc (1993) Mathematica, version 2.1. Wolfram Research Inc

  • Wones DR, Burns R, Carroll B (1971) Stability and properties of annite. Trans Am Geophys Union 52:369–370

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Dachs, E. Annite stability revised. 1. Hydrogen-sensor data for the reaction annite = sanidine + magnetite + H2 . Contr. Mineral. and Petrol. 117, 229–240 (1994). https://doi.org/10.1007/BF00310865

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00310865

Keywords

Navigation