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Alkaline Earth Transition Metal Antimonides AT<sub>4</sub>Sb<sub>12</sub> (A = Ca, Sr, Ba; T = Fe, Ru, Os) with LaFe<sub>4</sub>P<sub>12</sub>‐Structure
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Citations
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References
1994
Year
Materials ScienceInorganic ChemistryTransition Metal ChalcogenidesEngineeringTheoretical Inorganic ChemistryTransition MetalsApplied PhysicsCondensed Matter PhysicsQuantum MaterialsSolid-state ChemistryFunctional MaterialsChemistryInorganic MaterialCrystallographyRuthenium CompoundsSrsb 2
Abstract The title compounds were prepared by reaction of CaSb 2 , SrSb 2 , or BaSb 3 with the transition metals and antimony in sealed silica tubes. They crystallize with the cubic LaFe 4 P 12 ‐structure, which was refined from single‐crystal X‐ray data of CaFe 4 Sb 12 , SrRu 4 Sb 12 , and BaRu 4 Sb 12 to residuals of R = 0.014, 0.016, and 0.014, respectively. The thermal parameters of the alkaline earth ions increase with decreasing ionic size. The SbSb distances are greater in the iron compound than they are in the two ruthenium compounds. This is rationalized to be due to a larger portion of electrons in antibonding SbSb states in the iron compound.
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