地学前缘 ›› 2021, Vol. 28 ›› Issue (6): 179-186.DOI: 10.13745/j.esf.sf.2021.1.55

• 绿色提钾新工艺 • 上一篇    下一篇

基于Pitzer模型预测Na-K-Ca-Mg-Cl-H2O溶液的密度

路淼1,2, 李东东1, 李武1, 董亚萍1, 胡斌1,*   

  1. 1.中国科学院 青海盐湖研究所 中国科学院盐湖资源综合高效利用重点实验室/青海省盐湖资源化学重点实验室, 青海 西宁 810008;
    2.中国科学院大学, 北京 100049
  • 收稿日期:2021-01-08 修回日期:2021-02-16 出版日期:2021-11-25 发布日期:2021-11-25
  • 通讯作者: *胡 斌(1980—),男,副研究员,硕士生导师,主要从事溶液热力学模型研究。 E-mail:hubin@isl.ac.cn
  • 作者简介:路 淼(1996—),女,硕士研究生,物理化学专业。E-mail:lumiao@isl.ac.cn
  • 基金资助:
    国家重点研发计划项目(2017YFC0602805); 中国科学院国际伙伴计划项目(122363KYSB20190033)

Density prediction for the Na-K-Ca-Mg-Cl-H2O system using the Pitzer model

LU Miao1,2, LI Dongdong1, LI Wu1, DONG Yaping1, HU Bin1,*   

  1. 1. CAS Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources/Qinghai Provincial Key Laboratory of Resources and Chemistry of Salt Lake, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2021-01-08 Revised:2021-02-16 Online:2021-11-25 Published:2021-11-25

摘要: 天然水体系的体积性质与压力、温度、组成的相关性(PVTx性质)研究在地球化学、盐湖化工等领域有广泛的应用。密度是卤水最基本的体积性质,不仅可以通过实验测定,还可以用理论模型进行预测。建立富钾卤水密度与组成、温度的关联模型有助于认识钾在复杂卤水中的富集、迁移规律。为了构建基于Pitzer离子相互作用模型的卤水密度预测方法,本文用高精度振荡管密度计测定了常压下KCl、CaCl2纯盐溶液以及最高离子强度为11.8 mol·kg-1的混合溶液在283~323 K下的密度,用所测得的密度通过Pitzer离子相互作用模型拟合得到多温下Pitzer单电解质参数和Pitzer混合参数。用Pitzer模型参数计算了Na-K-Ca-Mg-Cl-H2O体系293~313 K的密度,计算密度值与实验值的相对偏差在±0.25%以内,计算的结果整体上要优于文献值,文献在计算中均未考虑Pitzer混合参数项。结果表明,K、Ca、Cl离子间的相互作用对于Na-K-Ca-Mg-Cl-H2O溶液的密度有显著的影响,本文获得的Pitzer参数反映了这些离子间的相互作用,可用于计算含有K、Ca、Cl离子的复杂卤水密度的预测。

关键词: 密度, 天然水, KCl, CaCl2, Pitzer离子相互作用模型

Abstract: PVTx properties of natural water are widely used in geochemistry and salt lake industry. By establishing the correlation between density, composition, temperature and pressure of potassium-rich brine, one can better understand the enrichment and migration of potassium in complex brine systems. In order to construct a prediction model for brine density based on the Pitzer model, densities of KCl and CaCl2 aqueous solutions and their mixtures were measured by vibrating-tube densitometry. The concentrations of single solute solutions were near saturation, and ionic strengths of aqueous mixtures were from 1.8 to 11.8 mol·kg-1. The Pitzer single electrolyte parameters and Pitzer mixing parameters at various temperatures between 283-323 K were obtained by Pitzer ion interaction model fitting using the measured densities, and the Pitzer volumetric parameters were obtained by fitting the volumetric Pitzer model to the experimental data. Densities of the Na-K-Ca-Mg-Cl-H2O hexary system over the temperature range of 293-313 K were calculated. The calculated density was in good agreement with the experimental results, with the relative error within 0.25%. The results show that ionic interactions had a significant effect on the density of the hexary system. The Pitzer parameters obtained in this paper reflect the interactions between these ions and can be used to make density predictions for complex brines containing K, Ca and Cl ions.

Key words: density, natural water, KCl, CaCl2, Pitzer ion interaction model

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