Evolution of the Ni2+ Environment During the Formation of a MgO-Al2O3-SiO2 Glass-Ceramic: A Combined XRD and Diffuse Reflectance Spectroscopy Approach

被引:15
|
作者
Dugue, Aymeric [1 ]
Cormier, Laurent [1 ]
Dargaud, Olivier [1 ,2 ]
Galoisy, Laurence [1 ]
Calas, Georges [1 ]
机构
[1] Univ Paris 06, CNRS, Inst Mineral & Phys Milieux Condenses, F-75005 Paris, France
[2] Cite Ceram, F-92310 Sevres, France
关键词
NEAR-INFRARED EMISSION; SILICATE GLASS; CATION DISTRIBUTION; CRYSTALLIZATION BEHAVIOR; ALUMINOSILICATE GLASSES; STRUCTURAL ENVIRONMENT; TEMPERATURE-DEPENDENCE; CORDIERITE GLASSES; RIETVELD METHOD; MELT SYSTEMS;
D O I
10.1111/j.1551-2916.2012.05421.x
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The effect of the addition of NiO on the crystallization mechanisms has been studied for SiO2-Al2O3-MgO glass-ceramics. A detailed Rietveld analysis has been made to determine the chemical composition and the cation distribution in the spinel phase and the evolution of Ni2+ coordination site using diffuse reflectance spectroscopy. Powder X-ray diffraction (XRD) results show the formation of beta-quartz and spinel and the nickel fraction in the spinel phase decreasing as the plateau temperature increases. The determination of cation distribution in spinel using XRD reveals a preference of Ni2+ and Al3+ for octahedral sites and an increasing proportion of Ni2+ in tetrahedral sites for heat treatments at high temperature (1100 degrees C-1200 degrees C). Diffuse reflectance spectroscopy shows that Ni2+ is mainly fivefold coordinated in the starting glass, playing an important role in the crystallization of the spinel phase and it confirms the presence of tetrahedral and octahedral Ni2+ in the glass-ceramics. The combination of these two techniques also indicates a chemical heterogeneity of spinel crystals with Ni2+-rich and Mg2+-rich zones.
引用
收藏
页码:3483 / 3489
页数:7
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