Phase Equilibrium in the System LiAlSiO4‐NaAlSiO4‐SiO2
Phase Equilibrium in the System LiAlSiO4‐NaAlSiO4‐SiO2
复制标题
DOI：
10.1111/j.1151-2916.1985.tb15279.x
复制
发表时间：
1985-02
影响因子：
3.9
通讯作者：
William B. Badger;F. A. Hummel
中科院分区：
文献类型：
--
作者：
William B. Badger;F. A. Hummel
锂霞石、锂辉石、钾霞石、霞石和钠长石的存在是众所周知的。为了建立LiAlSiO_4-NaAlSiO_4-SiO_2系统的相图，研究了高SiO_2平衡和LiAlSi_2O_6-NaAlSi_3O_8、LiAlSi_2O_6-NaAlSiO_4、LiAlSiO_4-NaAlSiO_4和LiAlSiO_4-NaAlSi_3O_8截面。LiAlSi 2 O 6-NaAlSi 3 O 8、LiAlSi 2 O 6-NaAlSiO 4和LiAlSiO 4-NaAlSiO 4的连接在大气压下低至800°C下建立。
The existence of eucryptite, spodumene, carnegieite, nepheline, and albite is very well known. To establish the phase diagram of the system LiAlSiO4-NaAlSiO4-SiO2, high-SiO2 equilibria and the sections LiAlSi2O6-NaAlSi3O8, LiAlSi2O6-NaAlSiO4, LiAlSiO4-NaAlSiO4, and LiAlSiO4-NaAlSi3O8were examined. The joins LiAlSi2O6-NaAlSi3O8, LiAlSi2O6-NaAlSiO4, and LiAlSiO4-NaAlSiO4 were established down to 800°C at atmospheric pressure.