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  • 1
    Online Resource
    Online Resource
    Walter de Gruyter GmbH ; 2023
    In:  Zeitschrift für Kristallographie - Crystalline Materials Vol. 238, No. 5-6 ( 2023-05-25), p. 151-166
    In: Zeitschrift für Kristallographie - Crystalline Materials, Walter de Gruyter GmbH, Vol. 238, No. 5-6 ( 2023-05-25), p. 151-166
    Abstract: Single crystals of five (Al,Ge)-mullites incorporating Pb, and four of which also incorporating foreign cations (Fe,Cr,Nd,Sm) were grown by flux techniques in a PbO-MoO 3 flux. They were characterized by scanning electron microscopy, electron microprobe analyses, single-crystal X-ray diffraction. In addition, the refractive indices of mullite containing Nd were determined by spindle-stage optical investigations. Careful inspection of the single-crystal X-ray diffraction data revealed that weak superstructure reflections observed in all doped crystals violating the reflection conditions can be attributed to λ/2 contributions in the primary X-ray beam. Consequently, all crystal structures were refined in space group Pbam , thus avoiding a symmetry lowering to a noncentrosymmetric subgroup as done in earlier work on a (Al,Ge)-mullite doped with Pb and Nd (Saalfeld & Klaska, Z. Kristallogr. 1985, 172, 129–133). The following phases with chemical compositions used in the refinements were obtained: undoped mullite (Al 4.50 Ge 1.50 O 9.75 ; a = 7.6559(4) Å, b = 7.7763(4) Å, c = 2.9233(2) Å, V = 174.04(2) Å 3 ); (Pb,Fe)-doped mullite (Pb 0.02 Fe 0.68 Al 3.95 Ge 1.37 O 9.70 ; a = 7.7125(7) Å, b = 7.8527(7) Å, c = 2.9528(2) Å, V = 178.83(3) Å 3 ); (Pb,Cr)-doped mullite (Pb 0.01 Cr 0.63 Al 3.90 Ge 1.47 O 9.75 ; a = 7.6917(6) Å, b = 7.8168(6) Å, c = 2.9522(2) Å, V = 177.50(2) Å 3 ); (Pb,Nd)-doped mullite (Pb 0.06 Nd 0.02 Al 4.82 Ge 1.18 O 9.69 ; a = 7.6585(7) Å, b = 7.7666(7) Å, c = 2.9164(3) Å, V = 173.47(3) Å 3 ); (Pb,Sm)-doped mullite (Pb 0.06 Sm 0.02 Al 4.55 Ge 1.45 O 9.79 ; a = 7.6563(3) Å, b = 7.7873(3) Å, c = 2.9236(1) Å, V = 174.31(1) Å 3 ); Pb is only incorporated into the crystal structure when a co-dopant element is present. Then it resides together with Nd or Sm in the oxygen-vacancy sites created by the formation of triclusters of AlO 4 and GeO 4 tetrahedra. In the case of (Pb,Fe)-doped mullite, Fe shares the same position as Al and Ge. In contrast to the (Al,Si)-mullites, Ge is located in both tetrahedral sites T and T*. The occupancies follow a substitution scheme according to Pb q (Nd,Sm) r (Cr,Fe) z Al 4+2 v − z Ge 2−2 v O 10− v + q +3/2 r . With v = number of vacancies, such a mullite can be understood as a “stuffed mullite” derived from a related “open mullite” (no vacancies filled with large cations) of composition (Cr,Fe) z Al 4+2 v − z Ge 2−2 v O 10− v and then “stuffed” with q Pb 2+ + r (Nd 3+ ,Sm 3+ ) formula units where concurrently the number of available O3-vacancies is reduced by q + 3/2 r units of extra oxygen. Thus, charge compensation upon incorporation of Pb 2+ and (Nd,Sm) 3+ is achieved by adding the amount of oxygen corresponding to the oxidation state of divalent Pb 2+ and trivalent rare-earth elements. Based on this description, the maximum number of large cations which can be stuffed into the mullite structure can directly be calculated from the v -value of the related “open mullite”. In contrast, the smaller cations Fe 3+ and Cr 3+ are directly substituting Al 3+ . In the stuffed mullites, Pb and (Nd,Sm) could not be distinguished and were refined with a mixed occupancy on the same site. In addition to structure analysis, refractive indices of (Pb,Nd)-mullite were determined by immersion methods using a micro-refractometer spindle stage yielding n x = 1.697(3), n y = 1.708(3), and n z = 1.710(3) and 2 V z = 122(4)°. The mean refractive index corresponds closely to the corresponding parameter calculated from the chemical composition whereas it would be significantly off if the extra cations were ignored, thus representing an independent evidence for the incorporation of Pb and Nd into the crystal structure.
    Type of Medium: Online Resource
    ISSN: 2194-4946 , 2196-7105
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    Language: English
    Publisher: Walter de Gruyter GmbH
    Publication Date: 2023
    SSG: 13
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  • 2
    In: Crystal Growth & Design, American Chemical Society (ACS), Vol. 16, No. 8 ( 2016-08-03), p. 4411-4420
    Type of Medium: Online Resource
    ISSN: 1528-7483 , 1528-7505
    Language: English
    Publisher: American Chemical Society (ACS)
    Publication Date: 2016
    detail.hit.zdb_id: 2048329-6
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  • 3
    In: European Journal of Mineralogy, Copernicus GmbH, Vol. 32, No. 6 ( 2020-12-17), p. 673-673
    Type of Medium: Online Resource
    ISSN: 1617-4011
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
    detail.hit.zdb_id: 1000286-8
    detail.hit.zdb_id: 2039451-2
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  • 4
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    Online Resource
    Mineralogical Society of America ; 2015
    In:  American Mineralogist Vol. 100, No. 7 ( 2015-07), p. 1493-1501
    In: American Mineralogist, Mineralogical Society of America, Vol. 100, No. 7 ( 2015-07), p. 1493-1501
    Type of Medium: Online Resource
    ISSN: 0003-004X
    RVK:
    Language: English
    Publisher: Mineralogical Society of America
    Publication Date: 2015
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    detail.hit.zdb_id: 2045960-9
    SSG: 13
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  • 5
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    Copernicus GmbH ; 2020
    In:  European Journal of Mineralogy Vol. 32, No. 2 ( 2020-03-11), p. 235-249
    In: European Journal of Mineralogy, Copernicus GmbH, Vol. 32, No. 2 ( 2020-03-11), p. 235-249
    Abstract: Abstract. A single crystal (∼ 20 µm × 20 µm × 330 µm) of mullite-2c, a natural polytype of mullite, was separated from a radially grown cluster of acicular crystals from Ettringer Bellerberg (Quarternary Eifel volcanic fields, Germany). The chemical composition determined from electron microprobe analysis (EMPA) is Na0.01Mg0.05Al8.52Fe0.293+Si3.13Ti0.02O19.55, corresponding to x=0.22(8) in the generalised mineral formula My+Mgz2+M8+4x+y-2z3+M4-4x-y+z4+O20-2x. Only Fe3+ as foreign cation was considered in the refined structure model, partially replacing Al3+ in the octahedral chains. A crystal of a similar type, though exhibiting a significantly different composition with x=0.02, was first described in 2015, tentatively named “sillimullite” by Fischer et al. (2015). This crystal and our new sample have similar structural properties, now classified as a polytype of mullite, designated mullite-2c. Single-crystal X-ray diffraction showed that the mullite-2c crystal investigated here exhibits partial Si ∕ Al ordering in the double chains of (Si,Al)O4 tetrahedra in contrast to the sample described in 2015 as being completely ordered. The ordering in mullite-2c results in a doubled c lattice parameter with respect to mullite. It crystallises in space group Pnam, with cell parameters for the new sample of a=7.5432(5) Å, b=7.7048(5) Å, c=5.7965(3) Å, V=336.89(6) Å3 and Z=1. X-ray powder diffraction data are presented with a detailed discussion of the differences between the diffraction patterns of sillimanite, mullite and mullite-2c. Crystals of mullite-2c are translucent to lightly violet, they possess a vitreous lustre and the calculated density is 3.199 g cm−3. The optical character is biaxial (+), with refractive indices determined by spindle-stage microscopy of nx=1.6673, ny=1.6687 and nz=1.680(4) (adjusted to conform to 2VZ=39(4)∘). Applying the Gladstone–Dale approach, the compatibility index is 0.007, representing superior compatibility. In terms of chemical composition and structural features mullite-2c is an outstanding example of mullite-type compounds falling into the postulated miscibility gap between sillimanite and mullite. Its crystal structure combines characteristics from both mullite (oxygen vacancies, triclusters of tetrahedral building units) and sillimanite (high degree of Si ∕ Al ordering in the tetrahedral building units, causing the doubled c parameter). The lattice parameters (normalised to 1c) of the new sample lie between those of sillimanite and 3 / 2 mullite; the chemical composition is close to 3 / 2 mullite and thus differs significantly from the silica-rich composition of the species previously determined by Fischer et al. (2015), indicating a relatively large compositional variation.
    Type of Medium: Online Resource
    ISSN: 1617-4011
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
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  • 6
    In: Zeitschrift für Kristallographie - Crystalline Materials, Walter de Gruyter GmbH, Vol. 235, No. 11 ( 2020-11-26), p. 533-551
    Abstract: Single crystals of ABW-type CsAlTiO 4 ( CAT ), CsFeTiO 4 ( CFT ), CsGaTiO 4 ( CGT ), and ANA-type CsTi 1.1 Si 1.9 O 6.5 ( CST ) were grown and characterized by electron microprobe analyses, single-crystal X-ray diffraction, thermal analyses, and spindle-stage optical investigations to determine the electronic polarizability of 4-coordinated Ti 4+ , α ( [4] Ti 4+ ). The crystal structure of CAT was confirmed to crystallize in the highest possible topological symmetry Imma ( a  = 8.9677(2) Å, b  = 5.7322(1) Å, c  = 9.9612(3) Å) with tetrahedrally coordinated Al and Ti equally distributed on Wyckoff position 8i. Twinning by reticular merohedry with a twin index of 2 was observed for most of the crystals resulting in a hexagonal twin lattice ( a  = 11.487(3) Å, c  = 8.968(2) Å) with Laue symmetry 6 / mmm . Refractive indices measured by immersion methods on an untwinned specimen are n x  = 1.716(5), n y  = 1.725(2), and n z  = 1.727(1) with 2 V z  = 127.1(6)°. The diffraction patterns of CFT and CGT clearly showed superstructure reflections causing a symmetry lowering of index 4 with a transformation according to 2 a , b , c from Imma to Pmab w ith a  = 18.3054(7) Å, b  = 5.8083(2) Å, c  = 9.9938(4) Å for CFT , and a  = 18.2921(6) Å, b  = 5.7636(2) Å, c  = 9.9210(3) Å for CGT . Refractive indices for CGT are n x  = 1.750(3), n y  = 1.772(3), and n z  = 1.776(2) with 2 V z  = 132(1)°. The crystal structure of the ANA-type CsTi 1.1 Si 1.9 O 6.5 was confirmed to crystallize in space group Ia 3 ¯ $\overline{3}$ d ( a  = 13.8333(4) Å). The extra 0.5 O atoms are needed for charge compensation and to allow the sum of electronic polarizabilities to give a total electronic polarizability calculated from the refractive index n  = 1.718(4). The electronic polarizability of [4] Ti 4+ was calculated from the difference between the observed total polarizabilities (derived from the mean refractive indices of CAT and CGT ) and the sum of electronic polarizabilities of cations and anions omitting the polarizability of Ti resulting in α ( [4] Ti 4+ ) = 5.15(5) Å 3 .
    Type of Medium: Online Resource
    ISSN: 2196-7105 , 2194-4946
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    Language: English
    Publisher: Walter de Gruyter GmbH
    Publication Date: 2020
    SSG: 13
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  • 7
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    Online Resource
    Schweizerbart ; 2019
    In:  European Journal of Mineralogy Vol. 31, No. 2 ( 2019-06-07), p. 353-367
    In: European Journal of Mineralogy, Schweizerbart, Vol. 31, No. 2 ( 2019-06-07), p. 353-367
    Type of Medium: Online Resource
    ISSN: 0935-1221
    Uniform Title: Natural mullites: chemical composition, crystal structure, and optical properties
    RVK:
    Language: English , English
    Publisher: Schweizerbart
    Publication Date: 2019
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    detail.hit.zdb_id: 2039451-2
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  • 8
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    Online Resource
    International Union of Crystallography (IUCr) ; 2013
    In:  Acta Crystallographica Section A Foundations of Crystallography Vol. 69, No. a1 ( 2013-08-25), p. s443-s444
    In: Acta Crystallographica Section A Foundations of Crystallography, International Union of Crystallography (IUCr), Vol. 69, No. a1 ( 2013-08-25), p. s443-s444
    Type of Medium: Online Resource
    ISSN: 0108-7673
    Language: Unknown
    Publisher: International Union of Crystallography (IUCr)
    Publication Date: 2013
    detail.hit.zdb_id: 2020844-3
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  • 9
    Online Resource
    Online Resource
    Walter de Gruyter GmbH ; 2012
    In:  International Journal of Materials Research Vol. 103, No. 4 ( 2012-04-01), p. 402-407
    In: International Journal of Materials Research, Walter de Gruyter GmbH, Vol. 103, No. 4 ( 2012-04-01), p. 402-407
    Abstract: Synthetic mullites (Al 4+2 x Si 2 –2 x O 10 – x ) belong to one of the most important groups of ceramic materials. Their crystal structure consists of chains of edge-sharing AlO 6 octahedra interconnected by tetrahedral double chains of T O 4 ( T = Al, Si) tetrahedra. The occurrence of oxygen vacancies is associated with the formation of triclusters of T O 4 groups. The distribution of oxygen vacancies and the distribution of Al and Si on the tetrahedral sites are partially ordered yielding an incommensurately modulated crystal structure with satellite reflections in diffraction patterns. The number of symmetrically independent distribution patterns of oxygen vacancies is given for a 2 × 2 × 2 and a 3 × 3 × 2 superstructure model. Many other compounds have chain structures similar to mullite. These compounds are assigned to subgroups, all derived from a hypothetical tetragonal aristotype structure.
    Type of Medium: Online Resource
    ISSN: 2195-8556 , 1862-5282
    RVK:
    Language: English
    Publisher: Walter de Gruyter GmbH
    Publication Date: 2012
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    detail.hit.zdb_id: 2128058-7
    detail.hit.zdb_id: 203021-4
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  • 10
    Online Resource
    Online Resource
    Wiley ; 2014
    In:  Zeitschrift für anorganische und allgemeine Chemie Vol. 640, No. 15 ( 2014-12), p. 3088-3093
    In: Zeitschrift für anorganische und allgemeine Chemie, Wiley, Vol. 640, No. 15 ( 2014-12), p. 3088-3093
    Abstract: In Bragg–Brentano powder X‐ray diffraction, incompletely filled sample holders result in a significant loss of intensity for diffraction peaks at small 2θ angles due to shadowing of the diffracted beam by the sample holder. This has to be considered in crystal structure refinements for samples with diffraction peaks in the low 2θ range when shifts of sample height cannot be avoided. Herein a geometrically derived correction algorithm to account for the intensity loss as a function of shift in sample height is presented. The algorithms were verified based on a series of zeolite A diffraction patterns from samples with deliberately induced, well defined reductions in sample height.
    Type of Medium: Online Resource
    ISSN: 0044-2313 , 1521-3749
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2014
    detail.hit.zdb_id: 201094-X
    detail.hit.zdb_id: 1481139-X
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