Home Structural investigation of two synthetic warwickites: Undistorted orthorhombic MgScOBO3 and distorted monoclinic Mg0.76Mn1.24OBO3
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Structural investigation of two synthetic warwickites: Undistorted orthorhombic MgScOBO3 and distorted monoclinic Mg0.76Mn1.24OBO3

Published/Copyright: August 25, 2010
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Abstract

The Mg – Sc warwickite, MgScOBO3, is an example of a normal orthorhombic warwickite [Pnam, a = 9.490(1), b = 9.422(1), c = 3.2189(4) Å and Z = 4]. The structure has been refined to an R value of 0.043, using the 258 X-ray reflection intensities with I > 3 · σ(I) and sin θ/λ ≤ 0.63 Å−1. The ratios of divalent to trivalent ions (Mg2+:Sc3+) at the two different metal sites are about 1:3 and 3:1, respectively. The investigation yields improved structural data for the common warwickite structure type. The Mg – Mn warwickite, Mg0.76Mn1.24OBO3, represents the first example of a distorted warwickite structure [P21/a, a = 9.370(2), b = 9.279(2), c = 3.181(1) Å, β = 85.65(2)° and Z = 4]. The derived structural model has been refined to an R value of 0.048 for the 385 X-ray reflection intensities with I > 3 · σ(I) and sin θ/λ ≤ 0.65 Å−1. The lowering of the symmetry, from orthorhombic for normal warwickites to monoclinic, is apparently due to structural effects caused by the Mn3+ ions. The coordination octahedra around the main Mn3+ sites are elongated with four shorter coplanar Mn – O bonds of 1.88 to 1.99 Å and two longer ones of 2.25 and 2.34 Å. The distributions of divalent and trivalent ions in the metal positions are similar to those in common warwickites.

Published Online: 2010-08-25
Published in Print: 1989

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  1. Structural investigation of two synthetic warwickites: Undistorted orthorhombic MgScOBO3 and distorted monoclinic Mg0.76Mn1.24OBO3
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