方解石在h2o - KCl - NaCl - LiCl溶液中700°C和8kbar溶解度的实验测定

J. Eguchi
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引用次数: 1

摘要

在研究深层碳循环时,了解方解石和水溶液之间的相互作用是很重要的。本研究考察了方解石在700°C和8kbar的盐- h2o流体中的溶解度。研究的盐类包括NaCl、KCl、LiCl和CsCl。所有的实验都是在活塞缸装置中进行的。结果表明,方解石溶解度随盐浓度的增加而增加。数据成功地拟合为盐摩尔分数平方的简单函数。在一定的盐浓度下,随着盐阳离子尺寸的减小,溶解度增强增大。在多种盐混合的流体中进行实验,得出了简单的关系式,可用于预测在所研究条件下方解石在各种盐溶液中的溶解度。结果为将该方法扩展到不同的压力、温度和盐成分提供了基础。
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Experimental Determination of Calcite Solubility in H 2 O‐KCl‐NaCl‐LiCl Solutions at 700°C and 8 kbar
Understanding the interactions between calcite and aqueous solutions is important when studying the deep carbon cycle. The present study investigates the solubility of calcite in salt-H2O fluids at 700 °C and 8 kbar. The investigated salts included NaCl, KCl, LiCl, and CsCl. All experiments were conducted in a piston cylinder apparatus. The results show that calcite solubility increases with increasing concentration of any individual salt. The data were successfully fit to simple functions of the square of salt mole fraction. At a given salt concentration, the solubility enhancement increases with decreasing salt cation size. Experiments in the fluids with mixtures of multiples of salts were used to derive simple relations that can be used to predict calcite solubility in a wide range of salt solutions at the studied conditions. The results provide a basis for extending this approach to different pressures, temperatures, and salt compositions.
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