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  • 1
    Electronic Resource
    Electronic Resource
    Zweikernige Aniongruppen [Fe2F10]4- in der Kristallstruktur von Sr5Fe3F19Professor Hanskarl Müller-Buschbaum zum 60. Geburtstage gewidmet (1991)
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 597 (1991), S. 51-59 
    Details
    ISSN: 0044-2313
    Keywords: Pentastrontium-trifluoride-{di-μ-fluoro-bis[tetrafluoroferrate(III)]}-hemafluoroferrate(III), Sr5F3[Fe2F10][FeF6] ; preparation ; crystal structure ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Dinuclear Anion Groups [Fe2F10]4- in the Crystal Structure of Sr5Fe3F19At single crystals of Sr5Fe3F19 a X-ray structure determination in the tetragonal space group 14/m was performed (a = 1429.4(3), c = 730.7(3) pm; Z = 4. wR = 0.019 for 502 independent reflections). Within the structure there are isolated, but disordered dimeric anion groups of edge-sharing octahedra [Fe2F10]4- (average Fe—F = 193.3 pm, Fe—Fe = 319.1 pm). They are embedded in a framework of strontium ions (C.N. 8-10) and single FeF63- octahedra (Fe—F = 191.0 resp. 192.7 pm, if corrected for thermal motion). The strong relations to the crystal structure of BaTiF5 and to further related fluoride compounds are discussed.
    Notes: An Einkristallen von Sr5Fe3F19 wurde eine röntgenographische Strukturbestimmung in der tetragonalen Raumgruppe 14/m durchgeführt (a = 1429,4(3), c = 730,7(3) pm; Z = 4. wR = 0,019 für 502 unabhängige Reflexe). In der Struktur treten isolierte, aber fehlgeordnete dimere Aniongruppen kantenverknüpfter Oktaeder [Fe2F10]4- auf (Mittelwert Fe—F = 193,3 pm, Fe—Fe = 319,1 pm). Sie sind eingebettet in ein Gerüst von Strontiumionen (KZ 8-10) und FeF63--Einzeloktaedern (Fe—F = 191,0 bzw. 192,7 pm, wenn für die thermische Schwingung korrigiert wird). Die engen Beziehungen zur Kristallstruktur von BaTiF5 und zu weiteren verwandten Fluorverbindungen werden diskutiert.
    Additional Material: 2 Ill.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1002/zaac.19915970108
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  • 2
    Electronic Resource
    Electronic Resource
    Die Kristallstrukturen der Weberite Na2CuScF7 und Na2ZnAlF7 (1994)
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 620 (1994), S. 1692-1697 
    Details
    ISSN: 0044-2313
    Keywords: Sodium copper scandium fluoride ; sodium zinc aluminium fluoride ; weberite structure ; crystal structure determination ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: The Crystal Structures of the Weberites Na2CuScF7 and Na2ZnAlF7At single crystals of the orthorhombic weberites Na2CuScF7 (Pmnb, Z = 4) and Na2ZnAlF7 (Imma, Z = 4) X-ray structure determinations were performed. Na2CuScF7 (Na2ZnAlF7): a = 726.0 (709.2), b = 1053.4 (1009.2), c = 765.8 (733.7) pm; R1 = 0.030 (0.042) for 887 (363) observed and independent reflections. The resulting average distances of the octahedrally coordinated metal atoms are: Cu—F = 200.7 pm, Sc—F = 201.7 pm; Zn—F = 198.8 pm, Al—F = 180.1 pm. Some structural relations and the variation in the bridge angles of the corner-sharing octahedra are discussed.
    Notes: An Einkristallen der orthorhombischen Weberite Na2CuScF7 (Pmnb, Z = 4) und Na2ZnAlF7 (Imma, Z = 4) wurden röntgenographische Strukturbestimmungen durchgeführt. Na2CuScF7 (Na2ZnAlF7): a = 726,0 (709,2), b = 1053,4 (1009,2), c = 765,8 (733,7) pm; R1 = 0,030 (0,042) für 887 (363) beobachtete und unabhängige Reflexe. Die resultierenden mittleren Abstände für die oktaedrisch koordinierten Metallatome sind: Cu—F = 200,7 pm, Sc—F = 201,7 pm; Zn—F = 198,8 pm, Al—F = 180,1 pm. Die Stukturverhältnisse und die Unterschiede in den Brückenwinkeln der eckenverknüpften Oktaeder werden diskutiert.
    Additional Material: 1 Ill.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1002/zaac.19946201005
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  • 3
    Electronic Resource
    Electronic Resource
    Tetragonale Cyanoelpasolithe: Die Kristallstrukturen von [N(CH3)4]2KMn(CN)6 und [N(CH3)4]2RbCo(CN)6Professor Helmut Köhler in memoriam. (1991)
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 600 (1991), S. 239-248 
    Details
    ISSN: 0044-2313
    Keywords: Cyano-elpasolites ; bis(-tetramethylammonium) alkali hexacyanometallates ; preparation ; crystal structures ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Tetragonal Cyano-Elpasolites: The Crystal Structures of [N(CH3)4]2KMn(CN)6 and [N(CH3)4]2RbCo(CN)6The tetragonal bis(-tetramethylammonium)-alkali-hexacyanometallates [N(CH3)4]2KMn(CN)6 (a = 884.8(2), c = 1222.2(6) pm) and [N(CH3)4]2RbCo(CN)6 (a = 884.7(1), c = 1233.1(2) pm) were prepared in the form of single crystals and their structures determined by X-ray methods (wR = 0.050 and 0.047 for 486 and 463 independent reflections, respectively; space group 14/m, Z = 2). The average distances in the resulting elpasolite structure, which is but slightly tetragonally distorted by small ferro-rotative displacements of the [M(CN6]3-) octahedra (Mn—C = 201.8, C—N = 115.6, K—N = 307.1 pm resp. Co—C = 190.7, C—N = 114.8, Rb—N = 320.1 pm), seem a bit enlarged if compared to related cyano complexes. Reasons for this are discussed using a tolerance factor concept for cyanoepasolites.
    Notes: Die tetragonalen Bis(-tetramethylammonium)-Alkali-Hexacyanometallate [N(CH3)4]2KMn(CN)6 (a = 884.8(2), c = 1222,2(6) pm) und [N(CH3)4]2RbCo(CN)6 (a = 884,7(1), c = 1233,1(2) pm) wurden in Form von Einkristallen dargestellt und röntgenographisch ihre Strukturen bestimmt (wR = 0,050 bzw. 0,047 für 486 bzw. 463 unabhängige Reflexe; Raumgruppe 14/m, Z = 2). Die mittleren Abstände in der resultierenden Elpasolithstruktur, die durch geringe ferrorotative Drehung der [M(CN)6]3--Oktaeder nur wenig tetragonal verzerrt ist (Mn—C = 201,8, C—N = 115,6, K—N = 307,1 pm bzw. Co—C = 190,7, C—N = 114,8, Rb—N = 320,1 pm), erscheinen leicht vergrößert im Vergleich zu Werten die in verwandten Cyanokomplexen beobachtet wurden. Gründe dafür werden im Rahmen einer Toleranzfaktorbetrachtung für Cyano-Elpasolithe diskutiert.
    Additional Material: 3 Ill.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1002/zaac.19916000133
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  • 4
    Electronic Resource
    Electronic Resource
    Structure of Na2Fe2F7 and structural relations in the family of weberites Na2MIIMIIIF7 (1993)
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 619 (1993), S. 1909-1919 
    Details
    ISSN: 0044-2313
    Keywords: Sodium iron fluoride ; weberite structure ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Struktur von Na2Fe2F7 und Strukturbeziehungen in der Weberitfamilie Na2MIIMIIIF7Die gemischtvalente Verbindung Na2Fe2F7 kristallisiert im monoklinen Weberit-Typ von Na2CuFeF7-II (M-II), Raumgruppe C2/c, Z = 16, a = 12,676, b = 7,422, c = 24,710 Å, β = 99,97°. Die Verfeinerung mit F2-Daten ergab wR(F2) = 0,117 für alle 2 645 Reflexe, R = 0,057 für 1 258 Reflexe mit Fo 〉 4σ(F). Auf der Grundlage dieser und anderer neuer Einkristalluntersuchungen werden die Strukturen der Weberite Na2MIIMIIIF7 in vier Haupttypen eingeteilt: O-I ist der „klassische“ orthorhombische Weberit (RG Imma), wie er im Mineral Na2MgAlF7 auftritt, und von dem sich zwei niedriger symmetrische Varianten, O-II (Na2CuCrF7-Typ) und O-III (Na2NiInF7), ableiten. Der zweite M-I und dritte M-II Typ sind monoklin (z. B. Na2CuFeF7-I and -II), der vierte Typ T ist trigonal (Na2MnFeF7). Die strukturellen Verwandtschaften innerhalb der Weberitfamilie werden diskutiert und die Zusammenhänge aufgezeigt, die es erlauben, diese Weberite ebenso wie die Pyrochlore als Subtraktionsabkömmlinge des Fluorittyps zu betrachten.
    Notes: The mixed valence compound Na2Fe2F7 crystallizes in the monoclinic weberite structure of the Na2CuFeF7-II type (M-II), space group C2/c, Z = 16, a = 12.676, b = 7.422, c = 24.710 Å, β = 99.97°. Refinement on F2 led to wR(F2) = 0.117 for all 2 645 reflections, R = 0.057 for 1 258 refl. with Fo 〉 4σ(F). On the basis of this and other recent single crystal investigations the structures of weberites Na2MIIMIIIF7 are classified in four main structure types: O-I is the ‘classical’ orthorhombic weberite type (S.G. Imma) encountered e.g. in the mineral Na2MgAlF7, from which two lower symmetric variants O-II (Na2CuCrF7 type) and O-III (Na2NiInF7) are deriving. The second M-I and third M-II basic type are monoclinic (e. g. Na2CuFeF7-I and -II), the fourth type T is trigonal (Na2MnFeF7). The structural relations within the weberite family are discussed and the connections established, which allow to regard these weberites as well as the pyrochlores as subtraction derivatives of the fluorite type.
    Additional Material: 10 Ill.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1002/zaac.19936191115
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