journal article·1997-01-01Open access

Crystal Structure, Magnetic Order, and Vibrational Behavior in Iron Rare-Earth Borates

J. A. Campá, C. Cascales, E. Gutiérrez-Puebla, M. A. Monge, I. Rasines, C. Ruíz-Valero

Chemistry of Materials· Volume 9· Issue 1

Abstract

Crystals of Fe 3 R(BO 3 ) 4 (R = Y, La, Nd) have been grown. Their structure and properties show close relations. The structures of these materials have been established by single-crystal X-ray diffraction. They crystallize in the huntite, CaMg 3 (CO 3 ) 4, structure type, trigonal system, space group R 32 (No. 155), Z = 3, with unit-cell parameters (Å) a = 9.592(1), 9.578(1), and 9.563(2) and c = 7.597(7), 7.605(3), and 7.575(2), for R = La, Nd, and Y 0.5 Bi 0.5, respectively. They contain RO 6 trigonal prisms and smaller FeO 6 octahedra forming layers and giving rise to Fe−R distances of ≃3.78 Å. RO 6 polyhedra are interconnected within the layers by corner sharing with triangular BO 3 groups of two types and FeO 6 octahedra. FeO 6 octahedra form 1D helicoidal chains with relatively short Fe−Fe distances, ≃3.18 Å. The temperature dependence of the magnetic susceptibility from 350 to 1.8 K for Fe 3 R(BO 3 ) 4 shows two maxima at about 260 and 35 K and, for R = Nd, another maximum at 6 K. The presence of magnetic order is attributed to magnetic Fe−Fe or Fe−O−Fe interactions. Infrared spectra in the range 4000−240 cm -1 show the ν 1, ν 3, and ν 4 IR-active bands of the B(1)O 3 3- triangular groups as well as ν 2 of less symmetrical B(2)O 3 3- .
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Research context

OpenAlex topics: Crystal Structures and Properties · Advanced Condensed Matter Physics · Radioactive element chemistry and processing

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Affiliations

Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, 28040 Madrid, and Instituto de Ciencia de Materiales, CSIC, Cantoblanco, 28049 Madrid, Spain

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