硅酸铝
拉曼光谱
遗传算法
地质学
作文(语言)
光谱学
矿物学
硅酸铝钙
钙
地球化学
化学
材料科学
冶金
物理
催化作用
有机化学
光学
进化生物学
量子力学
生物
语言学
哲学
作者
Daniel R. Neuville,Laurent Cormier,Dominique Massiot
出处
期刊:Chemical Geology
[Elsevier BV]
日期:2006-05-01
卷期号:229 (1-3): 173-185
被引量:350
标识
DOI:10.1016/j.chemgeo.2006.01.019
摘要
The structure and properties of glasses and melts in the CaO–Al2O3–SiO2 (CAS) system play an important role in earth and material sciences. Aluminum has a crucial role in this ternary system, and its environment is still questioned. In this paper, we present new results using Raman spectroscopy and 27Al Nuclear Magnetic Resonance on CAS glasses obtained by classic and rapid quenching methods. We propose an Al/Si tetrahedral distribution in the glass network in different Qn species. In this system, we show that Al and Si are mainly in Q4 species along the join R=CaO/Al2O3=1, and in depolymerized Q2 and Q3 units at high CaO content for other joins (R=1.57 and 3). Five- ([5]Al) and six-fold ([6]Al) coordinated aluminum can be detected in the peraluminous glasses (R 1), except for glasses with low silica and high CaO content. The presence of [5]Al is related to viscous flow mechanisms while, in highly depolymerized glasses, the absence of [5]Al may indicate different mechanisms for melts to flow. This systematic study on the CAS system modifies the simple picture of aluminosilicate glasses, and the existence of [5]Al should be included by geochemists, geophysicists and glass scientists to model appropriately the physical properties of aluminosilicate glasses and melts.
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