Hydrothermal synthesis, structural characterization and magnetic studies of the new pillared microporous ammonium Fe(III) carboxyethylphosphonate: [NH4][Fe2(OH){O3P(CH2)2CO2}2]
Creators
- 1. Instituto de Quimica Organometalica 'E. Moles', Departamento de Quimica Organica e Inorganica, Facultad de Quimica, c/Julian Claveria 8, Universidad de Oviedo, E-33006 Oviedo, Asturias (Spain)
- 2. Istituto di Cristallografia-CNR, Via Amendola 122, I-70125 Bari (Italy)
- 3. Istituto di Struttura della Materia-CNR, Sez. Montelibretti, Via Salaria km. 29.5, C.P. 10, I-00016 Monterotondo Staz., Rome (Italy)
- 4. Dipartimento di Chimica, Universita di Roma 'La Sapienza' P.le A. Moro, 00185 Rome (Italy)
Description
The preparation by hydrothermal reaction and the crystal structure of the iron(III) carboxyethylphosphonate of formula [NH4][Fe2(OH){O3P(CH2)2CO2}2] is reported. The green-yellow compound crystallizes in the monoclinic system, space group Pc(n.7), with the following unit-cell parameters: a=7.193(3)A, b=9.776(3)A, c=10.17(4)A and β=94.3(2) deg. It shows a typical layered hybrid organic-inorganic structure featuring an alternation of organic and inorganic layers along the a-axis of the unit cell. The bifunctional ligand [O3P(CH2)2CO2]3- is deprotonated and acts as a linker between adjacent inorganic layers, to form pillars along the a-axis. The inorganic layers are made up of dinuclear Fe(III) units, formed by coordination of the metal ions with the oxygen atoms originating from the [O3P-]2- end of the carboxyethylphosphonate molecules, the oxygen atoms of the [-CO2]- end group of a ligand belonging to the adjacent layer and the oxygen atom of the bridged OH group. Each Fe(III) ion is six-coordinated in a very distorted octahedral environment. Within the dimer the Fe-Fe separation is found to be 3.5A, and the angle inside the [Fe(1)-O(11)-Fe(2)] dimers is ∼124 deg. The resulting 3D framework contains micropores delimited by four adjacent dimers in the (bc) planes of the unit cell. These holes develop along the a-direction as tunnel-like pores and [NH4]+ cations are located there. The presence of the μ-hydroxo-bridged [Fe(1)-O(11)-Fe(2)] dimers in the lattice is also responsible for the magnetic behavior of the compound at low temperatures. The compound contains Fe3+ ions in the high-spin state and the two Fe(III) ions are antiferromagnetic coupled. The J/k value of -16.3K is similar to those found for other μ-hydroxo-bridged Fe(III) dimeric systems having the same geometry
Additional details
Identifiers
- DOI
- 10.1016/j.jssc.2004.10.047;
- PII
- S0022-4596(04)00586-9;
Publishing Information
- Journal Title
- Journal of Solid State Chemistry
- Journal Volume
- 178
- Journal Issue
- 1
- Journal Page Range
- p. 306-313
- ISSN
- 0022-4596
- CODEN
- JSSCBI
INIS
- Country of Publication
- United States
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 37034200
- Subject category
- S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY;
- Descriptors DEI
- ANTIFERROMAGNETISM; DIMERS; HIGH SPIN STATES; HYDROTHERMAL SYNTHESIS; IRON COMPLEXES; IRON IONS; LAYERS; LIGANDS; MAGNETIC PROPERTIES; MONOCLINIC LATTICES; PHOSPHONATES; SPACE GROUPS; X RADIATION
- Descriptors DEC
- CHARGED PARTICLES; COMPLEXES; CRYSTAL LATTICES; CRYSTAL STRUCTURE; ELECTROMAGNETIC RADIATION; ENERGY LEVELS; IONIZING RADIATIONS; IONS; MAGNETISM; ORGANIC COMPOUNDS; ORGANIC PHOSPHORUS COMPOUNDS; PHYSICAL PROPERTIES; RADIATIONS; SYMMETRY GROUPS; SYNTHESIS; TRANSITION ELEMENT COMPLEXES
Optional Information
- Copyright
- Copyright (c) 2004 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.