RARE-EARTH AND URANIUM TRANSITION-METAL PNICTIDES WITH LAFE4P12 STRUCTURE

Citation
Cbh. Evers et al., RARE-EARTH AND URANIUM TRANSITION-METAL PNICTIDES WITH LAFE4P12 STRUCTURE, Journal of alloys and compounds, 224(2), 1995, pp. 184-189
Citations number
22
Categorie Soggetti
Chemistry Physical","Metallurgy & Metallurigical Engineering","Material Science
ISSN journal
09258388
Volume
224
Issue
2
Year of publication
1995
Pages
184 - 189
Database
ISI
SICI code
0925-8388(1995)224:2<184:RAUTPW>2.0.ZU;2-N
Abstract
The new compounds NdFe4Sb12, SmFe4Sb12, EuFe4Sb12 and SmRu4Sb12 were p repared by reaction of the binary lanthanoid antimonides LnSb or EuSb2 respectively, with the transition metals and antimony in sealed silic a tubes. Single-crystal structure refinements of NdFe4Sb12 as well as of the previously reported compounds EuFe4P12, UFe4P12, EuRu4Sb12 and NdOs4Sb12 led to residuals of R=0.014, 0.023, 0.013, 0.025 and 0.042 r espectively. Systematic differences in the interatomic distances of Ce Fe4P12, EuFe4P12 and ThFe4P12 suggest that the Fermi level cuts throug h a phosphorus-phosphorus antibonding band. The thermal parameters of the rare earth components increase with the size of their transition m etal-pnictogen cages. The cell volumes of the LaFe4P12 type pnictides suggest that cerium and europium have intermediate valencies. In agree ment with the higher electronegativity of phosphorus, cerium is the mo st tetravalent in the phosphides and europium is the most divalent in the antimonides.