SOLID-SOLUTE PHASE-EQUILIBRIA IN AQUEOUS-SOLUTION .7. A REINTERPRETATION OF MAGNESIAN CALCITE STABILITIES

被引：17

作者：

KONIGSBERGER, E

GAMSJAGER, H

机构：

[1] Abteilung für Physikalische Chemie, Montanuniversität Leoben, Franz-Josef-Strasse 18

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1992年 / 56卷 / 11期

关键词：

D O I：

10.1016/0016-7037(92)90020-J

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：

It is proposed to model magnesian calcites thermodynamically as dilute solid solutions of MgCO3 in CaCO3 according to the Unified Interaction Parameter Formalism (BALE and PELTON, Met. Trans. A 21A, 1997-2002, 1990). In this case both stoichiometric saturation and precipitation data of synthetic magnesian calcites taken from literature can consistently be explained.

引用

页码：4095 / 4098

页数：4

共 18 条

[1]

[Anonymous], 1980, NEUES JB MINERAL ABH

[2] THE UNIFIED INTERACTION PARAMETER FORMALISM - THERMODYNAMIC CONSISTENCY AND APPLICATIONS [J].