Crystal structure of K0.75[FeII 3.75FeIII 1.25(HPO3)6]- 0.5H2O, an open-framework iron phosphite with mixed-valent FeII/FeIII ions

Single crystals of the title compound, potassium hexaphosphitopentaferrate( II,III) hemihydrate, K0.75[FeII 3.75FeIII 1.25(HPO3)6] 0.5H2O, were grown under mild hydrothermal conditions. The crystal structure is isotypic with Li1.43[FeII 4.43FeIII 0.57(HPO3)6] 1.5H2O and (NH4)2[FeII 5(HPO3)6] and exh...

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Detalles Bibliográficos
Autores: Serrano Larrea, Edurne, Mesa Rueda, José Luis, Legarra Sáez, Estíbaliz, Aguayo Urquijo, Andrés Tomás, Arriortua Marcaida, María Isabel
Tipo de recurso: artículo
Fecha de publicación:2016
País:España
Institución:Universidad del País Vasco
Repositorio:Addi. Archivo Digital para la Docencia y la Investigación
OAI Identifier:oai:addi.ehu.eus:10810/28706
Acceso en línea:http://hdl.handle.net/10810/28706
Access Level:acceso abierto
Palabra clave:crystal structure determination
iron phosphite
Mössbauer spectroscopy
Descripción
Sumario:Single crystals of the title compound, potassium hexaphosphitopentaferrate( II,III) hemihydrate, K0.75[FeII 3.75FeIII 1.25(HPO3)6] 0.5H2O, were grown under mild hydrothermal conditions. The crystal structure is isotypic with Li1.43[FeII 4.43FeIII 0.57(HPO3)6] 1.5H2O and (NH4)2[FeII 5(HPO3)6] and exhibits a [FeII 3.75FeIII 1.25(HPO3)6]0.75 open framework with disordered K+ (occupancy 3/4) as counter-cations. The anionic framework is based on (001) sheets of two [FeO6] octahedra (one with point group symmetry 3.. and one with point group symmetry .2.) linked along [001] through [HPO3]2 oxoanions. Each sheet is constructed from 12-membered rings of edge-sharing [FeO6] octahedra, giving rise to channels with a radius of ca 3.1 A ˚ where the K+ cations and likewise disordered water molecules (occupancy 1/4) are located. O O contacts between the water molecule and framework O atoms of 2.864 (5) A ˚ indicate hydrogen-bonding interactions of medium strength. The infrared spectrum of the compound shows vibrational bands typical for phosphite and water groups. The Mössbauer spectrum is in accordance with the presence of FeII and FeIII ions.