TY - JOUR
T1 - Rodalquilarite Revisited
T2 - The Hydrothermal Synthesis and Structural Reinvestigation of H3Fe2(TeO3)4Cl
AU - Feger, Christopher R.
AU - Kolis, Joseph W.
AU - Gorny, Krzysztof
AU - Pennington, Charles
N1 - Funding Information:
CRF thanks Dr. George L. Schimek for many valuable discussions. The work at Clemson University was supported by the National Science Foundation under Grant CHE-9102548, and the work at The Ohio State University was supported by the National Science Foundation under Grant DMR9357600 and by the U.S. Department of Energy, Midwest Superconductivity Consortium, under Contract DEFG02-90ER45427.
PY - 1999/3
Y1 - 1999/3
N2 - The known mineral rodalquilarite, H3Fe2(TeO3)4Cl, was obtained as high quality single crystals via hydrothermal reactions. This material crystallizes in the triclinic space group,P1, with cell constants ofa=5.103(2) Å,b=6.653(2) Å,c=9.012(3) Å,α=73.40(2)°,β=78.03(2),γ=76.76(2),V=282.1(2) Å3and was obtained from an NH4Cl solution that was heated at 375°C for 4 days. A detailed structural characterization was performed (R=0.039,Rw=0.050) and showed that this material is based on layers consisting of edge-sharing FeO6octahedra which are interconnected by TeO3pyramids which are completed by the presence of a terminal hydrogen atom. Additionally, a second set of TeO3pyramids attached to the FeO6octahedra are linked across the layers by a shared hydrogen atom. The layers are held together only through these O-H-O interactions and additional weak Te-Cl interactions. In this study, we compare this structure to a previous report of rodalquilarite and a reported triclinic form of Fe2Te4O11, which may have been misidentified and is also the title compound. In addition, we have obtained the band gap of this material by diffuse reflectance spectroscopy and find it to be a wide band gap (Eg=2.51eV) material. The DC magnetic susceptibility was also obtained and showed that the title compound is antiferromagnetic with aTNof 29 K.
AB - The known mineral rodalquilarite, H3Fe2(TeO3)4Cl, was obtained as high quality single crystals via hydrothermal reactions. This material crystallizes in the triclinic space group,P1, with cell constants ofa=5.103(2) Å,b=6.653(2) Å,c=9.012(3) Å,α=73.40(2)°,β=78.03(2),γ=76.76(2),V=282.1(2) Å3and was obtained from an NH4Cl solution that was heated at 375°C for 4 days. A detailed structural characterization was performed (R=0.039,Rw=0.050) and showed that this material is based on layers consisting of edge-sharing FeO6octahedra which are interconnected by TeO3pyramids which are completed by the presence of a terminal hydrogen atom. Additionally, a second set of TeO3pyramids attached to the FeO6octahedra are linked across the layers by a shared hydrogen atom. The layers are held together only through these O-H-O interactions and additional weak Te-Cl interactions. In this study, we compare this structure to a previous report of rodalquilarite and a reported triclinic form of Fe2Te4O11, which may have been misidentified and is also the title compound. In addition, we have obtained the band gap of this material by diffuse reflectance spectroscopy and find it to be a wide band gap (Eg=2.51eV) material. The DC magnetic susceptibility was also obtained and showed that the title compound is antiferromagnetic with aTNof 29 K.
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U2 - 10.1006/jssc.1998.8102
DO - 10.1006/jssc.1998.8102
M3 - Article
AN - SCOPUS:0000318638
SN - 0022-4596
VL - 143
SP - 254
EP - 259
JO - Journal of Solid State Chemistry
JF - Journal of Solid State Chemistry
IS - 2
ER -