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- W2113992972 startingPage "1643" @default.
- W2113992972 abstract "L'addition d'oxydes d'alcalins a la composition d'un verre silicate cause la disruption de la trame siliceuse et la formation d'atomes d'oxygene non chevauchants, rattaches a seulement un atome de Si, et donc des especes Q n . Les compositions de verre siliceux lithiniferes se comportent differemment des verres contenant un autre alcalin. L'addition de Li 2 O aux compositions a base de silicate et de germanate genere des groupes Q 2 a faible teneur en Li. De plus, la formation preferentielle d'un tel groupe est encore plus marquee pour les compositions a base de germanate que pour celles a base de silicate. Nous preconisons un mecanisme impliquant la liaison du Li a une paire d'atomes d'oxygene non chevauchants, faisant donc partie de groupes adjacents de tetraedres Q 2 , assurant ainsi une coordinence quatre du Li, dans un agencement planaire carre." @default.
- W2113992972 created "2016-06-24" @default.
- W2113992972 creator A5042315614 @default.
- W2113992972 creator A5079969043 @default.
- W2113992972 date "2005-10-01" @default.
- W2113992972 modified "2023-10-13" @default.
- W2113992972 title "THE STRUCTURE OF LITHIUM-CONTAINING SILICATE AND GERMANATE GLASSES" @default.
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- W2113992972 doi "https://doi.org/10.2113/gscanmin.43.5.1643" @default.
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