硅酸铝
拉曼光谱
地质学
铝
无定形固体
光谱学
协调数
矿物学
猝灭(荧光)
三元运算
分析化学(期刊)
离子
化学
材料科学
结晶学
冶金
荧光
物理
催化作用
有机化学
光学
计算机科学
量子力学
色谱法
程序设计语言
生物化学
作者
Daniel R. Neuville,Laurent Cormier,Dominique Massiot
出处
期刊:Chemical Geology
[Elsevier BV]
日期:2006-03-14
卷期号:229 (1-3): 173-185
被引量:442
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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