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Understanding the Formation of CaAl2Si2O8 in Melilite-Based Glass-Ceramics: Combined Diffractionand Spectroscopic Studies

机译:了解基于沸石的玻璃陶瓷中CaAl2Si2O8的形成:组合衍射和光谱学

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摘要

An assessment is undertaken for the formation of anorthite crystalline phase in a melilite-based glass composition (CMAS: 38.7CaO–9.7MgO–12.9Al2O3–38.7SiO2 mol %), used as a sealing material in solid oxide fuel cells, in view of the detrimental effect of anorthite on the sealing properties. Several advanced characterization techniques are employed to assess the material after prolonged heat treatment, including neutron powder diffraction (ND), X-ray powder diffraction (XRD), 29Si and 27Al magic-angle spinning nuclear magnetic resonance (MAS-NMR), and in situ Raman spectroscopy. ND, 29Si MAS-NMR, and 27Al MAS-NMR results revealed that both Si and Al adopt tetrahedral coordination and participate in the formation of the network structure. In situ XRD measurements for the CMAS glass demonstrate the thermal stability of the glass structure up to 850 °C. Further heat treatment up to 900 °C initiates the precipitation of melilite, a solid solution of akermanite/gehlenite crystalline phase. Qualitative XRD data for glass-ceramics (GCs) produced after heat treatment at 850 °C for 500 h revealed the presenceof anorthite along with the melilite crystalline phase. Rietveld refinementof XRD data indicated a high fraction of glassy phase (∼67%)after the formation of crystalline phases. The 29Si MAS-NMRspectra for the CMAS-GC suggest the presence of structural units inthe remaining glassy phase with a polymerization degree higher thandimer units, whereas the 27Al MAS-NMR spectra revealedthat most Al3+ cations exhibit a 4-fold coordination. Insitu Raman spectroscopy data indicate that the formation of anorthitecrystalline phase initiated after 240 h of heat treatment at 850 °Cowing to the interaction between the gehlenite crystals and the remainingglassy phase.
机译:考虑到在固体氧化物燃料电池中用作密封材料的一种基于陨石的玻璃成分(CMAS:38.7CaO–9.7MgO–12.9Al2O3–38.7SiO2 mol%)中钙长石结晶相的形成,进行了评估。钙长石对密封性能的不利影响。长时间热处理后,采用了几种先进的表征技术来评估材料,包括中子粉末衍射(ND),X射线粉末衍射(XRD), 29 Si和 27 Al魔角旋转核磁共振(MAS-NMR)和原位拉曼光谱。 ND, 29 Si MAS-NMR和 27 Al MAS-NMR结果表明,Si和Al均采用四面体配位并参与网络结构的形成。 CMAS玻璃的原位XRD测量表明,玻璃结构在高达850°C的温度下具有热稳定性。最高至900°C的进一步热处理会引发镁铝石沉淀,这是一种钙钛矿/方钠石结晶相的固溶体。在850°C热处理500 h后生产的玻璃陶瓷(GC)的定性XRD数据表明存在钙长石与陨石的结晶相。 Rietveld精致XRD数据表明玻璃态相的比例很高(〜67%)在形成结晶相之后。 29 Si MAS-NMRCMAS-GC的光谱表明存在结构单元剩余玻璃态的聚合度高于二聚体单元,而 27 Al MAS-NMR光谱显示大多数Al 3 + 阳离子表现出4倍配位。在原位拉曼光谱数据表明钙长石的形成850°C热处理240小时后,结晶相开始由于钠钙石晶体与其余的相互作用玻相。

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