化学和地球化学建模。298.15K下从低浓度到极高浓度(>35m)的二元氟化物系统的热力学模型

Stanislav Donchev, T. Tsenov, C. Christov
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引用次数: 3

摘要

在这项研究中,我们建立了经过验证的热力学模型,用于所有氟化物二元体系的溶液行为和固液平衡,并提供了活度数据。模拟研究的对象是298.15 K下低至极高浓度的1-1型(HF-H2O、NaF-H2O、KF-H2O、RbF-H2O和CsF-H2O)和1-2型(H2SiF6-H2O) 5个氟化物体系。模型是在Pitzer离子相互作用方法的基础上建立的。采用建议的平均活度系数(γ±)来构建HF-H2O体系的模型。为了参数化所有其他5个二元系统的模型,我们使用了所有可用的原始实验渗透系数数据(φ),适用于整个溶液浓度范围,直至饱和点。这里新开发的模型的预测与实验渗透系数数据非常一致,并且与从低到高浓度二元溶液的活度系数的建议一致:在HF-H2O中高达20 mol.kg - 1,在CsF-H2O中高达35.6 mol.kg - 1。根据评估的模型参数和使用实验m(sat)溶解度数据,确定了4种固相[NaF(s)、KF.2H2O(s)、RbF(s)和CsF(s)]的潮解相对湿度(DRH(%))和热力学溶解度产物(ln Kosp)。
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Chemical and geochemical modeling. Thermodynamic models for binary fluoride systems from low to very high concentration (> 35 m) at 298.15 K
Abstract In this study we developed well validated thermodynamic models for solution behavior and solid-liquid equilibrium for all fluoride binary systems, for which activity data are available. The subject of modeling study are 5 fluoride systems of the type 1-1 (HF-H2O, NaF-H2O, KF-H2O, RbF-H2O, and CsF-H2O) and one of 1-2 type (H2SiF6-H2O) from low to very high concentration at 298.15 K. Models are developed on the basis of Pitzer ion interactions approach. The recommendations on mean activity coefficients (γ±) have been used to construct the model for HF-H2O system. To parameterize models for all other 5 binary systems we used all available raw experimental osmotic coefficients data (φ) for whole concentration range of solutions, and up to saturation point. The predictions of new developed here models are in excellent agreement with experimental osmotic coefficients data, and with recommendations on activity coefficients in binary solutions from low to very high concentration: up to 20 mol. kg−1 in HF-H2O, and up to 35.6 mol.kg−1 in CsF-H2O. The Deliquescence Relative Humidity (DRH (%)) and thermodynamic solubility products (as ln Kosp) of 4 solid phases [NaF(s), KF.2H2O(s), RbF(s), and CsF(s)] have been determined on the basis of evaluated model parameters and using experimental m(sat) solubility data.
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