Abstract:Two glasses of the compositions 2 BaO - TiO2 - 2.75 GeO2 and 2 BaO – TiO2 –3.67 GeO2 (also known as BTG55) are annealed at temperatures from 680 to 970 °C to induce surface crystallization. The resulting samples are analyzed by X-ray diffraction (XRD) and scanning electron microscopy (SEM) including electron backscatter diffraction (EBSD). Ge-Fresnoite (Ba2TiGe2O8, BTG) is observed at the immediate surface of all samples and oriented nucleation is proven in both compositions. After a very fast kinetic selectio… Show more
“…20°. Considering this tilt, it can be concluded that the microstructure in Figure features Ba-fresnoite dendrites growing perpendicular to the surface, similar to the observations made for BT0.75G in a related glass-ceramic . Bulk nucleation was not detected in this BT3S glass-ceramics after the applied heat treatment.…”
Section: Results
and Discussionsupporting
confidence: 83%
“…Figure presents an SEM micrograph obtained from a cross section of the BT0.75S glass-ceramic showing an area where the growth fronts from the top and right side of the sample collided. In analogy to Ge-fresnoite, Ba-fresnoite shows no growth front interaction. Hence, the dendritic crystals growing in the BT0.75S-glass at 810 °C simply collide and prevent each other from further growth, similar to the observations made for Ge-fresnoite …”
Section: Results
and Discussionmentioning
confidence: 98%
“…While the growth front interactions of the related systems STS and BTG have been analyzed by SEM and EBSD to see whether the local growth velocity is increased, reduced, or unaffected, , this has not been done for Ba-fresnoite growing in glasses. Figure presents an SEM micrograph obtained from a cross section of the BT0.75S glass-ceramic showing an area where the growth fronts from the top and right side of the sample collided.…”
Section: Results
and Discussionmentioning
confidence: 99%
“…13 This observation is in contrast to the basic assumption of randomly oriented nuclei in the classical nucleation theory for glasses. Oriented nucleation has been described to occur in glass-ceramics containing Ba-fresnoite, 11,13 Sr-fresnoite, 14,15 or Ge-fresnoite. 16 It has also been detected in other systems during the surface crystallization of BaAl 2 B 2 O 7 , 17,18 diopside, 19 Sr 1−x/2 Al 2−x Si x O 4 (x = 0.9, 0.7, and 0.5), 20 walstromite, 21 probably ε-Y 2 Si 2 O 7 , as well as yttrium stabilized ZrO 2 22 and after the crystallization of mullite at the surface of a glass melt during cooling.…”
Glasses of the mol composition 2
BaO·TiO2·2
SiO2 + x SiO2 (with x = 0.0, 0.1, 0.2, 0.5, 0.75, 1.5, 2.0, and 3.0 mol) were
prepared, polished, and crystallized at 810 °C for 5 h or more.
All glasses showed the sole crystallization of Ba-fresnoite (Ba2TiSi2O8). The crystal orientations at
the immediate surfaces were analyzed by EBSD and showed that all glasses
exhibit a nonrandom orientation distribution, i.e., oriented nucleation
at the surface. While the glasses with x = 0.0, 0.1,
and 0.2 show rather broad orientation preferences in the form of c-axes tilted from the surface by roughly 10–50°,
the glasses with x = 1.5 or higher show discrete
textures where specific crystal orientations are significantly preferred
with orientation spreads of less than ±15°. While the glasses
with x = 0 and 0.1 show polygon crystals at the surface
and in the bulk, dendritic crystals are observed in the bulk of all
other analyzed compositions. Phase separation solely occurred in the
glass with x = 1.5 during the applied heat treatments.
“…20°. Considering this tilt, it can be concluded that the microstructure in Figure features Ba-fresnoite dendrites growing perpendicular to the surface, similar to the observations made for BT0.75G in a related glass-ceramic . Bulk nucleation was not detected in this BT3S glass-ceramics after the applied heat treatment.…”
Section: Results
and Discussionsupporting
confidence: 83%
“…Figure presents an SEM micrograph obtained from a cross section of the BT0.75S glass-ceramic showing an area where the growth fronts from the top and right side of the sample collided. In analogy to Ge-fresnoite, Ba-fresnoite shows no growth front interaction. Hence, the dendritic crystals growing in the BT0.75S-glass at 810 °C simply collide and prevent each other from further growth, similar to the observations made for Ge-fresnoite …”
Section: Results
and Discussionmentioning
confidence: 98%
“…While the growth front interactions of the related systems STS and BTG have been analyzed by SEM and EBSD to see whether the local growth velocity is increased, reduced, or unaffected, , this has not been done for Ba-fresnoite growing in glasses. Figure presents an SEM micrograph obtained from a cross section of the BT0.75S glass-ceramic showing an area where the growth fronts from the top and right side of the sample collided.…”
Section: Results
and Discussionmentioning
confidence: 99%
“…13 This observation is in contrast to the basic assumption of randomly oriented nuclei in the classical nucleation theory for glasses. Oriented nucleation has been described to occur in glass-ceramics containing Ba-fresnoite, 11,13 Sr-fresnoite, 14,15 or Ge-fresnoite. 16 It has also been detected in other systems during the surface crystallization of BaAl 2 B 2 O 7 , 17,18 diopside, 19 Sr 1−x/2 Al 2−x Si x O 4 (x = 0.9, 0.7, and 0.5), 20 walstromite, 21 probably ε-Y 2 Si 2 O 7 , as well as yttrium stabilized ZrO 2 22 and after the crystallization of mullite at the surface of a glass melt during cooling.…”
Glasses of the mol composition 2
BaO·TiO2·2
SiO2 + x SiO2 (with x = 0.0, 0.1, 0.2, 0.5, 0.75, 1.5, 2.0, and 3.0 mol) were
prepared, polished, and crystallized at 810 °C for 5 h or more.
All glasses showed the sole crystallization of Ba-fresnoite (Ba2TiSi2O8). The crystal orientations at
the immediate surfaces were analyzed by EBSD and showed that all glasses
exhibit a nonrandom orientation distribution, i.e., oriented nucleation
at the surface. While the glasses with x = 0.0, 0.1,
and 0.2 show rather broad orientation preferences in the form of c-axes tilted from the surface by roughly 10–50°,
the glasses with x = 1.5 or higher show discrete
textures where specific crystal orientations are significantly preferred
with orientation spreads of less than ±15°. While the glasses
with x = 0 and 0.1 show polygon crystals at the surface
and in the bulk, dendritic crystals are observed in the bulk of all
other analyzed compositions. Phase separation solely occurred in the
glass with x = 1.5 during the applied heat treatments.
“…4 indicate an oriented nucleation of ε-YS with the c-axis preferably parallel to the surface and of Y-ZrO 2 with a {111}-plane parallel to the surface. Oriented nucleation has currently been detected in more than five glass systems, most recently in Ge-fresnoite 43 where multiple phases showed up to three orientation preferences at the immediate surface after crystallization 43 . As the ε-YS dendrites in the EBSD-scan of Fig.…”
The crystallization behavior of a glass with the composition 54.7 SiO2·10.9 Al2O3·15.0 MgO·3.4 ZrO2·16.0 Y2O3 is studied using X-ray diffraction (XRD), scanning electron microscopy (SEM) including electron backscatter diffraction (EBSD) and (scanning) transmission electron microscopy [(S)TEM] including energy-dispersive X-ray spectrometry (EDXS). This glass shows the sole surface crystallization of four different yttrium silicates of the composition Y2Si2O7 (YS). The almost simultaneous but independent nucleation of α-, β-, δ-, and ε-YS at the surface is followed by growth into the bulk, where ε-YS quickly dominates a first crystallized layer. An accumulation of Mg at the growth front probably triggers a secondary nucleation of β-YS, which forms a thin compact layer before fragmenting into a highly oriented layer of fine grained crystals occupying the remaining bulk. The residual glass between the YS growth structures allows the crystallization of indialite, yttrium stabilized ZrO2 (Y-ZrO2) and very probably μ-cordierite during cooling. Hence, this glass basically shows the inverted order of crystallization observed in other magnesium yttrium alumosilicate glasses containing less Y2O3. An epitaxial relationship between Y-ZrO2 and ε-YS is proven and multiple twinning relationships occur in the YS phases.
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