Solubility of niobium in the system CaCO3-Ca(OH)2-NaNbO3 at 0.1 GPa pressure

被引:26
|
作者
Mitchell, RH
Kjarsgaard, BA
机构
[1] Lakehead Univ, Dept Geol, Thunder Bay, ON P7B 5E1, Canada
[2] Geol Survey Canada, Ottawa, ON K1A 0E8, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1007/s00410-002-0384-3
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Experimental data are presented for the solubility of NaNbO3 in the ternary system CaCO3-Ca(OH)(2)-NaNbO3 (or calcite-portlandite-lueshite) over the temperature range 500-950 degreesC at 0.1 GPa pressure. Near-liquidus phase relationships are given for the pseudo-binary join ([CaCO3](45)[Ca(OH)(2)](55))(100)-(-)(x)(NaNbO3)(x); (0 < x < 70 wt%). These data show the presence of a large field of calcite plus liquid and the absence of NaNbO3 as a primary liquidus phase until the melts contain greater than 60 wt% NaNbO3. The primary crystallization fields of calcite and NaNbO3 are separated by a steep thermal valley located at about 55 wt% NaNbO3. Quenched liquids contain calcite, portlandite, sodium carbonates and perovskite-structured calcium niobates. The maximum solubility of Nb2O5 in this system is estimated to be on the order of 48 wt% at 650 degreesC at 0.1 GPa pressure. The experiments show that perovskite-structured compounds rather than pyrochlore crystallize from these fluorine-free, water-rich melts.
引用
收藏
页码:93 / 97
页数:5
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