Experimental Investigation of Cation Exchange Equilibria of the Gallium Feldspar Solid Solution (K, Rb)GaSi3O8 with KCl–RbCl–H2O Fluids at 550°C and 1.5 kbar with Applications to the Description of the Properties of Solid Solutions with the Feldspar Structure

IF 1.1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
A. R. Kotelnikov, N. I. Suk, Z. A. Kotelnikova, G. M. Akhmedzhanova, N. A. Drozhzhina
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引用次数: 0

Abstract

Feldspars of the KGaSi3O8–RbGaSi3O8 series were synthesized at 550°C and 1.5 kbar, and their exchange reactions with 1 M KCl + 1 M RbCl solution were investigated. Using the experimental data, Margules parameters were calculated for the description of the excess mixing energies of the (K,Rb)GaSi3O8 solid solution: WG1 = WG2 = 4.46 ± 0.11 kJ/mol. We refined the unit-cell parameters of the solid solutions; the excess mixing volume is described by the Margules model: WV1 = 2.647 ± 0.05 and WV2 = –0.883 ± 0.04 cm3/mol. The results were compared with feldspars studied previously. Empirical relations were proposed for the calculation of the energy Margules model and unit-cell volumes for various minerals with the feldspar structure.

Abstract Image

镓长石固溶体(K, Rb)GaSi3O8与KCl-RbCl-H2O流体在550℃和1.5 kbar下阳离子交换平衡的实验研究及其在长石结构固溶体性质描述中的应用
在550℃、1.5 kbar条件下合成了KGaSi3O8-RbGaSi3O8系列长石,并对其与1 M KCl + 1 M RbCl溶液的交换反应进行了研究。利用实验数据,计算了描述(K,Rb)GaSi3O8固溶体的过量混合能的Margules参数:WG1 = WG2 = 4.46±0.11 kJ/mol。改进了固溶体的单元胞参数;过量混合体积用Margules模型描述:WV1 = 2.647±0.05,WV2 = -0.883±0.04 cm3/mol。结果与前人研究的长石进行了比较。提出了计算长石结构矿物的能量Margules模型和单位胞体体积的经验关系式。
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来源期刊
Petrology
Petrology 地学-地球科学综合
CiteScore
2.40
自引率
20.00%
发文量
27
审稿时长
>12 weeks
期刊介绍: Petrology is a journal of magmatic, metamorphic, and experimental petrology, mineralogy, and geochemistry. The journal offers comprehensive information on all multidisciplinary aspects of theoretical, experimental, and applied petrology. By giving special consideration to studies on the petrography of different regions of the former Soviet Union, Petrology provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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