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Crystal structure and properties of valleriite

Crystal structure and properties of valleriite

Günther Josef Redhammer (ORCID: 0000-0003-0996-3930)
  • Grant DOI 10.55776/P19762
  • Funding program Principal Investigator Projects
  • Status ended
  • Start June 1, 2007
  • End May 31, 2011
  • Funding amount € 204,866

Disciplines

Chemistry (15%); Geosciences (70%); Physics, Astronomy (15%)

Keywords

    Valleriite, Composite Crystal, Crystal Structure, Synthesis, Spectroscopy, Physical Properties

Abstract Final report

Valleriite is a relatively rare and unusual mineral, displaying a regular stacking of sulphide and hydroxide layers. The combination of two such entirely different building units is a peculiarity in several ways. Since the structural topology of the two layers is different, they only match conditionally in certain directions. Thus a regular alternating of the two different structures develops. Such materials are known as composite - crystals, a description of the atomic structure takes place in the multidimensional (3+n) space. Within the group of sulphides such composite - and also incommensurably modulated structures occur quite frequently and represent current research trends in modern crystallography. In addition the physical properties of valleriite and derived synthetic compounds promise to be of interest: it is the combination of the n-type semi-conducting chalcopyrite-type layer with the hydrogen and transition metal containing brucite layer which makes the material of interest, especially with respect to photo-electrochemical properties; a technical application may be possible. However, even basic physical properties of valleriite are unknown. The aim of the proposed research project is a comprehensive chemical and structural as well as a fundamental physical characterisation of natural and synthetically manufactured valleriite type materials. The determination of the parameters (P - T - X and fugacity) important for the synthesis of phase pure and well crystallized samples represents thereby an important project emphasis.

Valleriite is a relatively rare and unusual mineral, displaying a regular stacking of sulphide and hydroxide layers. The combination of two such entirely different building units is a peculiarity in several ways. Since the structural topology of the two layers is different, they only match conditionally in certain directions. Thus a regular alternating of the two different structures develops. Such materials are known as composite - crystals, a description of the atomic structure takes place in the multidimensional (3+n) space. Within the group of sulphides such composite - and also incommensurably modulated structures occur quite frequently and represent current research trends in modern crystallography. In addition the physical properties of valleriite and derived synthetic compounds promise to be of interest: it is the combination of the n-type semi-conducting chalcopyrite-type layer with the hydrogen and transition metal containing brucite layer which makes the material of interest, especially with respect to photo-electrochemical properties; a technical application may be possible. However, even basic physical properties of valleriite are unknown. The aim of the proposed research project is a comprehensive chemical and structural as well as a fundamental physical characterisation of natural and synthetically manufactured valleriite type materials. The determination of the parameters (P - T - X and fugacity) important for the synthesis of phase pure and well crystallized samples represents thereby an important project emphasis.

Research institution(s)
  • Universität Salzburg - 100%
International project participants
  • Werner Paulus, Université de Rennes I - France
  • Werner Treumann, Philipps-Universität Marburg - Germany
  • Georg Roth, Rheinisch-Westfälische Technische Hochschule - Germany
  • Joachik Mayer, Rheinisch-Westfälische Technische Hochschule Aachen - Germany

Research Output

  • 239 Citations
  • 8 Publications
Publications
  • 2010
    Title Nuclear and incommensurate magnetic structure of NaFeGe2O6 between 5 K and 298 K and new data on multiferroic NaFeSi2O6
    DOI 10.1007/s00269-010-0390-3
    Type Journal Article
    Author Redhammer G
    Journal Physics and Chemistry of Minerals
    Pages 139-157
  • 2010
    Title Thermal expansion and high-temperature P21/c–C2/c phase transition in clinopyroxene-type LiFeGe2O6 and comparison to NaFe(Si,Ge)2O6
    DOI 10.1007/s00269-010-0368-1
    Type Journal Article
    Author Redhammer G
    Journal Physics and Chemistry of Minerals
    Pages 685-704
  • 2007
    Title Yttrium pyrogermanate, Y2Ge2O7
    DOI 10.1107/s0108270107042825
    Type Journal Article
    Author Redhammer G
    Journal Acta Crystallographica Section C: Crystal Structure Communications
  • 2009
    Title The magnetic structure of clinopyroxene-type LiFeGe2O6 and revised data on multiferroic LiFeSi2O6
    DOI 10.1016/j.jssc.2009.06.013
    Type Journal Article
    Author Redhammer G
    Journal Journal of Solid State Chemistry
    Pages 2374-2384
  • 2008
    Title Synthetic aenigmatite analog Na2(Mn5.26Na0.74)Ge6O20: structure and crystal chemical considerations
    DOI 10.1107/s0108270107068011
    Type Journal Article
    Author Redhammer G
    Journal Acta Crystallographica Section C: Crystal Structure Communications
  • 2008
    Title Chromium-based clinopyroxene-type germanates NaCrGe2O6 and LiCrGe2O6 at 298 K
    DOI 10.1107/s0108270108037633
    Type Journal Article
    Author Redhammer G
    Journal Acta Crystallographica Section C: Crystal Structure Communications
  • 2008
    Title Magnetic ordering and spin structure in Ca-bearing clinopyroxenes CaM2+(Si, Ge)2O6, M=Fe, Ni, Co, Mn
    DOI 10.1016/j.jssc.2008.08.014
    Type Journal Article
    Author Redhammer G
    Journal Journal of Solid State Chemistry
    Pages 3163-3176
  • 2009
    Title Magnetic and nuclear structure and thermal expansion of orthorhombic and monoclinic polymorphs of CoGeO3 pyroxene
    DOI 10.1007/s00269-009-0335-x
    Type Journal Article
    Author Redhammer G
    Journal Physics and Chemistry of Minerals
    Pages 311-332

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