Mineralogical Journal
Online ISSN : 1881-4174
Print ISSN : 0544-2540
ISSN-L : 0544-2540
 
On variety of the Ca coordination in the incommensurate structure of synthetic iron-bearing åkermanite, Ca2(Mg0.55,Fe0.45)Si2O7.
Katsuhiro KUSAKAMasaaki OHMASAKenji HAGIYAKazuaki IISHINobuhiko HAGA
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1998 Volume 20 Issue 2 Pages 47-58

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Abstract

The incommensurate modulation in a synthetic iron-bearing åkermanite, Ca2(Mg, Fe)Si2O7, has been determined at room temperature by the five-dimensional refinements of the structure. The basic structure is tetragonal P-421m with unit-cell dimensions a=7.8679(3), c=5.0144(2)Å, V=310.41(2)Å3, Z=2, M=286.69, Dx=3.067Mg·m−3, MoKα with graphite monochromator, μ=3.199mm−1, F(000)=284.49, Mg/(Mg+Fe)=0.554(6), R=0.065 for 770 unique reflections. The modulated structure is also tetragonal PP4mgp-421m, k1=0.295(2)×(a*+b*), k2=0.295(2)×(-a*+b*), where k1, k2 are the wave vectors and a*, b* the reciprocal lattice vectors of the basic structure. R=0.136 for 3965 unique reflections. The modulation is caused mainly by the shifts of Ca and O atoms, and substitutional modulation at (Mg, Fe) sites was not detected in the present studies. Six-coordinated Ca forming a distorted oxygen octahedra exists in the modulated structure and most of them form clusters together with the flattened (Mg,Fe)O4 tetrahedra. The number of the clusters in the present material is less than that in Co-åkermanite. The reason may be attributed to the disorder of the modulation amplitudes and wavelength.

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© 1998 Japan Association of Mineralogical Sciences
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