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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: European Journal of Mineralogy, Copernicus GmbH, Vol. 32, No. 1 ( 2020-01-15), p. 27-40
    Abstract: Abstract. It is shown here that the H2O content of hydrous minerals can be determined from their mean refractive indices with high accuracy. This is especially important when only small single crystals are available. Such small crystals are generally not suitable for thermal analyses or for other reliable methods of measuring the amount of H2O. In order to determine the contribution of the H2O molecules to the optical properties, the total electronic polarizability is calculated from the anhydrous part of the chemical composition using the additivity rule for individual electronic polarizabilities of cations and anions. This anhydrous contribution is then compared with the total observed electronic polarizability calculated from the mean refractive index of the hydrous compound using the Anderson–Eggleton relationship. The difference between the two values represents the contribution of H2O. The amount can be derived by solving the equation αcalc=∑iniαicat+∑jαjo×10-NjVm1.2×nj+nW1.2+nw×αW for the number nw of H2O molecules per formula unit (pfu), with the electronic polarizabilities αcat for cations, the values N and αo describing the anion polarizabilities, the number n of cations and anions, and the molar volume Vm, using a value of αW=1.62 Å3 for the electronic polarizability of H2O. The equation is solved numerically, yielding the number nw of H2O molecules per formula unit. The results are compared with the observed H2O content evaluating 157 zeolite-type compounds and 770 non-zeolitic hydrous compounds, showing good agreement. This agreement is expressed by a factor relating the calculated to the observed numbers being close to 1 for the majority of compounds. Zeolites with occluded anionic or neutral species (SO3, SO4, CO2, or CO3) show unusually high deviations between the calculated and observed amount of H2O, indicating that the polarizabilities of these species should be treated differently in zeolites and zeolite-type compounds.
    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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  • 3
    In: Crystal Research and Technology, Wiley, Vol. 55, No. 8 ( 2020-08)
    Abstract: χ (3) ‐nonlinear optical interactions in two melilite‐type stimulated Raman scattering (SRS)‐active non‐centrosymmetric crystals, Ca 2 MgSi 2 O 7 and Ca 2 Ga 2 SiO 7 , formerly known as Nd 3+ ‐laser media, are presented. Under picosecond pumping at 1.064 and 0.532 µm cascaded and cross‐cascaded effects occur in these tetragonal silicates. Besides the SRS‐promoting phonon modes with energy of ω SRS1 ≈ 908 cm −1 and ω SRS2 ≈ 668 cm −1 for Ca 2 MgSi 2 O 7 , and ω SRS1 ≈ 720 cm −1 and ω SRS2 ≈ 550 cm −1 for Ca 2 Ga 2 SiO 7 , respectively, combined phonon modes are observed. For Ca 2 MgSi 2 O 7 new data in a broad wavelength range of refractive indices and their dispersion are given as well. The observed χ (3) ‐nonlinear properties expand the functionality of the studied silicates and foreshadow their use in self‐frequency Raman laser converters (self‐SRS lasers).
    Type of Medium: Online Resource
    ISSN: 0232-1300 , 1521-4079
    URL: Issue
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    Language: English
    Publisher: Wiley
    Publication Date: 2020
    detail.hit.zdb_id: 1480828-6
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  • 4
    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
    RVK:
    Language: English
    Publisher: Walter de Gruyter GmbH
    Publication Date: 2020
    SSG: 13
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