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  • Wiley-Blackwell  (2)
  • 1985-1989  (2)
  • 1989  (2)
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  • 1985-1989  (2)
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  • 1
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Synthesis, Characterization, and EPR Studies of Heteropoly Compounds with Iron(III) in Tetrahedral and Octahedral CoordinationThe heteropoly compounds H5[FeO4W12O36] · 6 H2O (a0 = 1216 pm), H3[Fe(OH)6Mo6O18] · 4 H2O, Na5[FeO4W12O36] · nH2O and FeH2[FeO4W12O36] · 17 H2O, for the first time obtained in this work by freeze-drying and characterized by means of chemical analysis, i.r. and u.v. spectroscopy, X-ray powder-photographs, and magnetic measurements, appear as suitable model systems for EPR investigations. They contain, like a number of known FeIII-heteropoly compounds, FeIII in FeO4 or/and FeO6 units, which are isolated from each other by structural reasons.In the Keggin-compounds M5[EIIIO4W12O36] · nH2O (I) (M = Na, Rb, TMA, TEA; E = Fe, Al, B) FeIII occupies slightly distorted tetrahedral positions (g′ ≍ 2), which are characterized by zfs-values of ≍ 10 mT and line widthes ΔB of 2.0⃛15 mT. Unlike as for I cations with different physico-chemical characteristics have only little effect on the FeIII-zfs. This holds for the Anderson-complexes M3[Fe(OH)6Mo6O18]·nH2O, (M = H, K, NH4, TMA; g′ ≍ 4.3 ΔB ≍ 67 mT) and for M5[SiO4W11O35FeO5(OH2)]·nH2O, (M = K, TMA; g′ = 4.3 ΔB = 26.5 mT). The FeO6 octahedra are more distorted than the FeO4 tetrahedra in I and therefore less susceptible for structural changes.
    Notes: Die mittels Gefriertrocknung erstmalig synthetisierten und strukturanalytisch charakterisierten Verbindungen H5[FeO4W12O36] · 6 H2O (a0 = 1216 pm), H3[Fe(OH)6Mo6O18] · 4 H2O, Na5[FeO4W12O36] · nH2O und FeH2[FeO4W12O36] · 17 H2O sind zusammen mit einer Reihe bekannter FeIII-haltiger Heteropolyverbindungen geeignete Modellsysteme für die EPR, da sie FeIII in räumlich voneinander weitgehend getrennten FeO4- oder/und FeO6-Struktureinheiten enthalten. In den Keggin-Verbindungen M5[EIIIO4W12O36] · nH2O (I) (M = Na, Rb, TMA, TEA; E = Fe, Al, B) besetzt FeIII gering verzerrte Tetraederplätze (g′ ≍ 2), die durch zfs-Beiträge von etwa 10 mT und Linienbreiten ΔB von 2,0 bis ≍ 15 mT charakterisiert sind. Sowohl in den Verbindungen vom Anderson-Typ M3[Fe(OH)6Mo6O18] · nH2O (M = H, K, NH4, TMA; g′ ≍ 4,3; ΔB ≍ 67 mT) als auch in M5[SiO4W11O35FeO5(OH2)] · nH2O (M = K, TMA; g′ = 4,3; ΔB = 26,5 mT) wirken sich Kationen mit unterschiedlichen physikalisch-chemischen Eigenschaften - anders als bei I - nur in geringem Maße auf die FeIII-zfs aus. Die FeO6-Oktaeder sind stärker verzerrt als die FeO4-Tetraeder in I und damit weniger strukturempfindlich.
    Additional Material: 2 Ill.
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  • 2
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 576 (1989), S. 215-224 
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Thermolysis of Potassium and Ammonium Pentafluorometallate Hydrates. An in situ-EPR StudyIn situ-EPR investigations on Fe3+ ions in K2AlF5 · H2O, (NH4)2[AlF5(H2O)], and (NH4)2[FeF5(H3O)] were carried out in the temperature range from 25°C to 230°C. The Fe3+ ions occupy in these compounds Al3+ sites with rhombic and axial symmetry. These Fe3+ ions are suszeptible for structural changes at the thermolysis. Simultaniously Fe—O—Fe species are formed, yielding autonomous phases in this process. The conclusions, done from EPR investigations agree with results of other methods (e.g. X-ray and thermal analysis) and complete them in unique manner.
    Notes: In situ-EPR-Untersuchungen von Fe3+-Ionen in K2AlF5 · H2O, (NH4)2[AlF5(H2O)] und (NH4)2[FeF5(H2O)] wurden im Temperaturbereich zwischen 25°C und 230°C durchgeführt. Dabei zeigte sich, daß Fe3+-Ionen in diesen Verbindungen Al3+-Gitterplätze rhombischer und axialer Symmetrie besetzen. Diese Fe3+-Ionen zeigen in empfindlicher Weise Strukturänderungen bei der Thermolyse an. Gleichzeitig entstehen bei diesem Prozeß Fe—O—Fe-Spezies in selbständigen Phasen. Die Ergebnisse zeigen, daß EPR-Untersuchungen zusätzliche Strukturaussagen liefern und so röntgenographische und andere Aussagen in spezifischer Weise ergänzen.
    Additional Material: 3 Ill.
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