Startseite Formation of clathrates Ba–M–Ge(M = Mn, Fe, Co)
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Formation of clathrates Ba–M–Ge(M = Mn, Fe, Co)

  • Andriy Grytsiv , Natalja Melnychenko-Koblyuk , Navida Nasir , Peter Rogl , Adriana Saccone und Harald Schmid
Veröffentlicht/Copyright: 11. Juni 2013
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Abstract

In order to define the ability of magnetic elements M = Mn, Fe, Co to stabilise clathrate structures, alloys of the Ba – M – Ge system were investigated in the as-cast state and after annealing at 700°C and 800°C by means of X-ray powder diffraction, light optical and electron-probe microanalysis. Temperatures of phase transformations were derived from differential thermal analysis. Results are summarised in (i) isothermal sections at 700°C and 800°C, (ii) solidus and liquidus surfaces covering the region of existence for both clathrate phases in these systems. Invariant reactions during crystallisation are presented in form of Schultz – Scheil diagrams.

In all three cases only limited solubility of the M element was found for clathrate IX (Ba6Ge25) i. e. the Ge-framework in the crystal structure of Ba6MxGe25 – x dissolves 0.6 atom of Mn, and about 1 atom of Fe and Co per unit cell. The maximum solubility of iron in clathrate type I (Ba8Ge46 – x) was found to be less than 0.5 Fe atom per unit cell, and clathrates with Mn and Co contain up to 1.0 and 2.5 atoms in the unit cell, respectively. Whilst Fe does not decrease the formation temperature of the clathrate phase, Mn and Co decrease it from 770°C (for binary Ba8Ge43) to 766°C and 749°C, respectively.


* Correspondence address, Prof. Peter Rogl Institute of Physical Chemistry, University of Vienna Währingerstraße 42, A-1090 Wien, Austria Tel.: +43 1 4277 52 456 Fax: +43 1 4277 95 245 E-mail:

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Received: 2008-11-17
Accepted: 2008-12-3
Published Online: 2013-06-11
Published in Print: 2009-02-01

© 2009, Carl Hanser Verlag, München

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