Skip to main content
Log in

Structure and crystal chemistry of hydrous wadsleyite, Mg1.75SiH0.5O4: possible hydrous magnesium silicate in the mantle transition zone

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

Abstract

The crystal structure of hydrous wadsleyite, Mg1.75SiH0.5O4 synthesized in an MA 8-type apparatus at conditions of 1300°C and 15.5 GPa, has been analyzed and refined in space group Imma, using the X-ray intensities measured on a 60X60X10 μm single crystal. The composition (Z=8) and unit cell are Mg1.74Si0.97H0.65O4 by E.P.M.A. analysis and a=5.663(1) Å, b= 11.546(2) Å, c=8.247(4) Å, V=539.2(5) Å3. The partial M-site occupancies were determined; vacancies associated with the incorporation of water are strongly concentrated on the Mg 3 site. The OH in the structure was confirmed by Raman and FTIR spectroscopies. The result of valence sum calculation based on the refined bond lengths indicates that O1 is a hydroxyl. The formula of hydrous wadsleyite can be expressed as Mg2-xSiH2xO4, where 0≤x≤0.25. When x=0.25, all of the O1 site is hydroxyl and the maximum solubility of 3.3 wt% H2O is realized. Structural relations to other dense hydrous phases are discussed.

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.

Institutional subscriptions

Similar content being viewed by others

References

  • Anderson DL (1970) Petrology of the mantle. Mineral Soc Amer Spec Pap 3:85–93

    Google Scholar 

  • Anderson OL, Nafe JE (1965) The bulk modulus-volume relationship for oxide compounds and related geophysical problems. J Geophys Res 70:3951–3963

    Google Scholar 

  • Bass JD, Kanzaki M, Howell DA (1991) Sound velocities and elastic properties of phase E: a high pressure hydrous silicae. EOS Trans Am Geophys Union 72:499

    Google Scholar 

  • Bina CR, Wood BJ (1987) Olivine-spinel transitions: experimental and thermodynamic constraints and implications for the nature of the 400-km seismic discontinuity. J Geophys Res 92:4853–4866

    Google Scholar 

  • Birch F (1961) The velocity of compressional waves in rocks to 10 kilobars, part 2. J Geophys Res 66:2199–2224

    Google Scholar 

  • Brown ID (1981) The bond-valence method: an empirical approach to chemical structure and bonding. In: O'Keeffe M, Navrotsky A (eds) Structure and bonding in crystals, Vol II, p. 1–30, Academic Press, New York

    Google Scholar 

  • Cromer DT, Waber JT (1974) Mean atomic scattering factors in electrons for free atoms and chemically significant ions. International Tables for X-ray Crystallography, Vol IV, Table 2.2 A, Birmingham, England

  • Downs JW (1989) Possible sites for protonation in β-Mg2SiO4 from an experimentally derived electrostatic potential. Am Mineral 74:1124–1129

    Google Scholar 

  • Finger LW, Hazen RM, Prewitt CT (1991) Crystal structure of Mg12Si4O19(OH)2 (phase B) and Mg14Si5O24 (phase Anh B). Am Mineral 76:1–7

    Google Scholar 

  • Finger LW, Hazen RM, Zhang J, Ko J, Navrotsky A (1993) The effect of Fe on the crystal structure of wadsleyite β(Mg1-xFex)2SiO4, 0.00 ≤x ≤0.40. Phys Chem Minerals 19:361–368

    Google Scholar 

  • Gasparik T (1993) The role of volatiles in the transition zone. J Geophys Res 98:4287–4299

    Google Scholar 

  • Hazen RM, Zhang J, Ko J (1990) Effects of Fe/Mg on the compressibility of synthetic wadsleyite: β-(Mg1-xFex)2SiO4 (x ≤0.25). Phys Chem Minerals 17:416–419

    Google Scholar 

  • Horiuchi H, Sawamoto H (1981) β-Mg2SiO4: single-crystal X-ray diffraction study. Am Mineral 66:568–575

    Google Scholar 

  • Horiuchi H, Morimoto N, Yamamoto K, Akimoto S (1979) Crystal structure of 2 Mg2SiO4·3 Mg(OH)2, a new high-pressure structure type. Am Mineral 64:593–598

    Google Scholar 

  • Inoue T (1994) Effect of water on melting phase relations and melt composition in the system Mg2SiO4-MgSiO3-H2O up to 15 GPa. Phys Earth Planet Inter 85:237–263

    Google Scholar 

  • Inoue T, Yurimoto H, Kudoh Y (1995) Hydrous modified spinel, Mg1.75SiH0.5O4: a new water reservoir in the mantle transition region. Geophys Res Let 22:117–120

    Google Scholar 

  • Jeanloz R, Thompson AB (1983) Phase transition and mantle discontinuities. Rev Geophys Space Phys 21:51–74

    Google Scholar 

  • Kohlstedt DL, Keppler H, Rubie DC (1994) Solubility of water in a, β and γ(Mg, Fe)2SiO4 at high pressures. EOS Trams Am Geophys Union 75:652

    Google Scholar 

  • Kudoh Y, Finger LW, Hazen RM, Prewitt CT, Kanzaki M, Veblen DR (1993) Phase E: a high pressure hydrous silicate with unique crystal chemistry. Phys Chem Minerals 19:357–360

    Google Scholar 

  • Kudoh Y, Nagase T, Ohta S, Sasaki S, Kanzaki M, Tanaka M (1994) Crystal structure and compressibility of superhydrous phase B, Mg20Si6H8O36. In: Schmidt SC, Shaner JW, Samara GA, Ross M (eds) High-Pressure Science and Technology-1993, pp. 469–472, American Institute of Physics

  • Kudoh Y, Nagase T, Sasaki S, Tanaka M, Kanzaki M (1995) Phase F, a new hydrous magnesium silicate synthesized at 1000 °C and 17 GPa: crystal structure and its estimated bulk modulus. Phys Chem Minerals 22: 295–299

    Google Scholar 

  • Martin RF, Donnay G (1972) Hydroxyl in the mantle. Am Mineral 57:554–570

    Google Scholar 

  • McMillan PF, Akaogi M, Sato RK, Poe B, Foley I (1991) Hydroxyl groups in β-Mg2SiO4. Am Mineral 76:354–360

    Google Scholar 

  • Moore PB, Smith JV (1970) Crystal structure of β-Mg2SiO4: Crystal-chemical and geophysical implications. Phys Earth Planet Inter 3:166–177

    Google Scholar 

  • Morimoto N, Akimoto S, Koto K, Tokonami M (1969) Modified spinel, beta-manganous orthogermanate: stability and crystal structure. Science 165:586–588

    Google Scholar 

  • Nakamoto K, Margoshes M, Rundle RE (1955) Stretching frequencies as a function of distances in hydrogen bonds. J Am Chem Soc 77:6480–6486

    Google Scholar 

  • Pacalo REG, Parise IB (1992) Crystal structure of superhydrous B, a hydrous magnesium silicate synthesized at 1400 °C and 20 GPa. Am Mineral 77:681–684

    Google Scholar 

  • Sawamoto H, Weidner DJ, Sasaki S, Kumazawa M (1984) Single crystal elastic properties of modified spinel (beta) phase of magnesium orthosilicate. Science 224:749–751

    Google Scholar 

  • Sawamoto H, Horiuchi H (1990) β(Mg0.9, Fe0.1)2SiO4: single crystal structure, cation distribution, and properties of coordination polyhedra. Phys Chem Minerals 17:293–300

    Google Scholar 

  • Smyth JR (1987) β-Mg2SiO4: a potential host for water in the mantle? Am Mineral 72:1051–1055

    Google Scholar 

  • Smyth JR (1994) A crystallographic model for hydrous wadsleyite (β-Mg2SiO4): an ocean in the Earth's interior? Am Mineral 79:1021–1024

    Google Scholar 

  • teXsan (1992) Crystal Structure Analysis Package, Molecular Structure Corporation, Texas, USA

  • Young TE, Green HW II, Hofmeister AM, Walker D (1993) Infrared spectroscopic investigation of hydroxyl in β(Mg, Fe)2SiO4 and coexisting olivine: implications for mantle evolution and dynamics. Phys Chem Minerals 19:409–422

    Google Scholar 

  • Yusa H, Inoue T (1994) Compressibility measurements of hydrous β-phase by X-ray diffraction study under high pressure. The 35th High Pressure Conference of Japan, Abstr:20

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Kudoh, Y., Inoue, T. & Arashi, H. Structure and crystal chemistry of hydrous wadsleyite, Mg1.75SiH0.5O4: possible hydrous magnesium silicate in the mantle transition zone. Phys Chem Minerals 23, 461–469 (1996). https://doi.org/10.1007/BF00202032

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00202032

Keywords

Navigation