The crystal structure of the elusive huemulite

The crystal structures of natural huemulite from the West Sunday mine, Utah, USA, and synthetic huemulite, Na4Mg(V10O 28)·24H2O, have been solved and refined to R 1 = 0.0313 (for 3535 unique F0 > AσF reflections) and 0.0246 (for 3672 unique F0 > 4σF reflections), respectively. Huemulit...

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Autor principal: Colombo, F.
Otros Autores: Baggio, R., Kampf, A.R
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2011
Acceso en línea:Registro en Scopus
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100 1 |a Colombo, F. 
245 1 4 |a The crystal structure of the elusive huemulite 
260 |c 2011 
270 1 0 |m Colombo, F.; CONICET-Cátedra de Geología General, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad National de Córdoba, Av. Vélez Sarsfield 1611, (X50I6GCA) Córdoba, Argentina 
506 |2 openaire  |e Política editorial 
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504 |a Hughes, J.M., Schindler, M., Francis, C.A., The C2/m disordered structure of pascoite, Ca3[V10 O28]17H2O: Bonding between structural units and interstitial complexes in compounds containing the [V10O 28]6- decavanadate polyanion (2005) Canadian Mineralogist, 43 (4), pp. 1379-1386 
504 |a Hughes, J.M., Schindler, M., Rakovan, J., Cureton, F.E., The crystal structure of hummerite, KMg(V5O 14)8H2O: Bonding between the [V10O 28]6- structural unit and the {K2Mg 2(H2O)16}6+ interstitial complex (2002) Canadian Mineralogist, 40 (5), pp. 1429-1435 
504 |a Hughes, J.M., Wise, W.S., Gunter, M.E., Morton, J.P., Rakovan, J., Lasalite, Na2Mg2[V10O 28]·20H2O, a new decavanadate mineral species from the Vanadium Queen mine, La Sal District, Utah: Description, atomic arrangement, and relationship to the pascoite group of minerals (2008) Can. Mineral., 46, pp. 1365-1372 
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504 |a Kampf, A.R., Steele, I.M., Magnesiopascoite, a new member of the pascoite group: Description and crystal structure (2008) Can. Mineral., 46, pp. 679-686 
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520 3 |a The crystal structures of natural huemulite from the West Sunday mine, Utah, USA, and synthetic huemulite, Na4Mg(V10O 28)·24H2O, have been solved and refined to R 1 = 0.0313 (for 3535 unique F0 > AσF reflections) and 0.0246 (for 3672 unique F0 > 4σF reflections), respectively. Huemulite is triclinic, space group P1̄, Z = 1; unit-cell dimensions of the natural sample are a 9.0453(2), b 11.3337(3),c 11.7372(8) Å, α 105.223(7), β 97.383(7), γ 100.790(7)°, V 1120.30(9) Å3, whereas those of the synthetic sample are a 9.0425(2), b 11.3303(2), c 11.7353(8) Å, α 105.222(7), β 97.377(7), γ 100.791(7)°, V 1119.47(8) Å3. The structure consists of decavanadate oxyanions (V10O28) 6- linked via an interstitial complex composed of isolated [Mg(H 2O)6]2+ octahedra and an [Na4(H 2O)14]4+ cationic group (defining an infinite zigzag chain). There are also four isolated H2O groups, two of them positionally disordered. All except four H atoms have been located, showing a network of hydrogen bonds that further links the interstitial complex and the structural unit, stabilizing the atomic arrangement. The Lewis acidity of the interstitial complex (0.18) is almost coincident with the upper limit of basicity of the structural unit (0.17), thus showing that the valencematching principle is maintained in this structure. It is probable that the X-ray pattern and the unit-cell dimensions in the original description of huemulite were measured using a mixture that included fully hydrated and partially dehydrated material. Huemulite is a member of the pascoite group, which is closely related to a synthetic family of general formula Na4M(V10O 28)·23H2O (M: Ni, Mg).The unit cell and atomic positions of huemulite are related to those of the synthetic family by the transformation matrix M = [100/011/011̄]. However, some of the symmetry restrictions (e.g., inversion centers, cell centering) present in huemulite are relaxed, with the consequence that fewer atoms are symmetry-related in the synthetic materials.  |l eng 
593 |a CONICET-Cátedra de Geología General, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad National de Córdoba, Av. Vélez Sarsfield 1611, (X50I6GCA) Córdoba, Argentina 
593 |a Departamento de Física, Lab. TANDAR, Comisión National de Energía Atómica, Av. Gral Paz 1499, (BI650KNA) San Martín, Buenos Aires, Argentina 
593 |a Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, United States 
690 1 0 |a DECAVANADATE 
690 1 0 |a HUEMULITE 
690 1 0 |a HYDROGEN BONDING 
690 1 0 |a PASCOITE FAMILY 
690 1 0 |a VALENCE-MATCHING PRINCIPLE 
690 1 0 |a ATOMIC ARRANGEMENT 
690 1 0 |a ATOMIC POSITIONS 
690 1 0 |a CATIONIC GROUPS 
690 1 0 |a DECAVANADATE 
690 1 0 |a HUEMULITE 
690 1 0 |a INTERSTITIAL COMPLEXES 
690 1 0 |a INVERSION CENTER 
690 1 0 |a LEWIS ACIDITY 
690 1 0 |a OXYANIONS 
690 1 0 |a PASCOITE 
690 1 0 |a SPACE GROUPS 
690 1 0 |a STRUCTURAL UNIT 
690 1 0 |a SYNTHETIC MATERIALS 
690 1 0 |a TRANSFORMATION MATRICES 
690 1 0 |a UNIT CELLS 
690 1 0 |a UNIT-CELL DIMENSIONS 
690 1 0 |a UPPER LIMITS 
690 1 0 |a UTAH , USA 
690 1 0 |a VALENCE-MATCHING PRINCIPLE 
690 1 0 |a X-RAY PATTERNS 
690 1 0 |a ZIGZAG CHAINS 
690 1 0 |a ATOMS 
690 1 0 |a HYDROGEN 
690 1 0 |a HYDROGEN BONDS 
690 1 0 |a LINEAR TRANSFORMATIONS 
690 1 0 |a CRYSTAL ATOMIC STRUCTURE 
690 1 0 |a CHEMICAL BONDING 
690 1 0 |a CRYSTAL CHEMISTRY 
690 1 0 |a CRYSTAL STRUCTURE 
690 1 0 |a HUEMULITE 
690 1 0 |a LATTICE DYNAMICS 
690 1 0 |a PASCOITE 
690 1 0 |a SYMMETRY 
690 1 0 |a UNITED STATES 
690 1 0 |a UTAH 
700 1 |a Baggio, R. 
700 1 |a Kampf, A.R. 
773 0 |d 2011  |g v. 49  |h pp. 849-864  |k n. 3  |p Can. Mineral.  |x 00084476  |w (AR-BaUEN)CENRE-833  |t Canadian Mineralogist 
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