4.6 Article

A new layered organically templated iron(II) phosphite, (C2H10N2) [Fe3(HPO3)4].: Hydrothermal synthesis, crystal structure and spectroscopic and magnetic properties

期刊

JOURNAL OF SOLID STATE CHEMISTRY
卷 177, 期 8, 页码 2705-2713

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jssc.2004.04.020

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hydrothermal synthesis; X-ray diffraction; IR; UV/vis; Mossbauer; magnetic behavior

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The (C2H10N2) [Fe-3(HPO3)(4)] compound has been synthesized by using mild hydrothermal conditions-under autogeneous pressure and the ethylenediamine molecule as templating agent. The compound crystallizes in the triclinic P (1) over bar space group with unit-cell parameters a = 5.416(1), b = 5.416(1), c = 13.977(2) Angstrom, alpha = 80.64(2), beta = 85.25(1), gamma = 60.03(1)degrees and Z = 1. The final R-factors were R-1 = 0.053 [wR(2) = 0.092]. The crystal structure is constructed of layers stacked along the c-axis. The sheets contain FeO6 octahedra linked by (HPO3)(2-) phosphite oxoanions to give rise to Fe3O12 trimeric units sharing faces. The IR spectrum shows the characteristic bands of the phosphite and ethylenediammonium ions. From the diffuse reflectance spectrum, the Dq parameter of 805 cm(-1) has been calculated for the iron(II) cation in slightly distorted octahedral geometry. The Mossbauer spectrum exhibits two doublets characteristic of two crystallographically independent iron(II) ions in octahedral symmetry. Magnetic measurements indicate the existence of antiferromagnetic interactions. (C) 2004 Elsevier Inc. All rights reserved.

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