一种预测高T、高P水离子热力学性质的新方法

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Andrey V. Plyasunov
{"title":"一种预测高T、高P水离子热力学性质的新方法","authors":"Andrey V. Plyasunov","doi":"10.1016/j.chemgeo.2025.122756","DOIUrl":null,"url":null,"abstract":"<div><div>Calculation of the molar standard state Gibbs energies of aqueous ions, <span><math><msubsup><mi>G</mi><mn>2</mn><mi>o</mi></msubsup></math></span>, at supercritical temperatures and pressures is a prerequisite for thermodynamic modeling of hydrothermal processes. Currently, such calculation is performed only with the well-known HKF model, and the development of alternative methods is highly desirable to avoid any possible bias. As a step in this direction, the author presents a novel “isochoric” method for predicting the Gibbs energies of aqueous ions up to high temperatures and pressures. The method is based on the analysis of the temperature dependence of the partial molar isochoric heat capacity of aqueous ions, <span><math><msubsup><mi>C</mi><mrow><mi>v</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>. Knowing <span><math><msubsup><mi>C</mi><mrow><mi>v</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>, one can compute the partial molar isobaric heat capacity <span><math><msubsup><mi>C</mi><mrow><mi>p</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>, provided that <span><math><msubsup><mi>V</mi><mn>2</mn><mi>o</mi></msubsup></math></span> is known as a function of <em>T</em> and <em>P</em>. Then the calculation of <span><math><msubsup><mi>G</mi><mn>2</mn><mi>o</mi></msubsup></math></span> can be performed by the traditional methods. The test of this method was performed using two literature formulations (Arcis et al., 2024; Marshall and Franck, 1981) for the ionization constant of water over wide ranges of temperature (273–1273 K) and water density ρ (up to ρ = 1.25 g cm<sup>−3</sup>), which allow computing all thermodynamic properties of a hypothetical HOH electrolyte. Using 4 parameters at most, it is possible to reproduce the water ionization constants recommended by either Arcis et al. (2024) or Marshall and Franck (1981) formulations at supercritical temperatures with deviations less than those of these formulations. It is expected that the proposed “isochoric” method deserves further investigation.</div></div>","PeriodicalId":9847,"journal":{"name":"Chemical Geology","volume":"682 ","pages":"Article 122756"},"PeriodicalIF":3.6000,"publicationDate":"2025-03-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A novel method for correlating/predicting the thermodynamic properties of aqueous ions at high T and P\",\"authors\":\"Andrey V. Plyasunov\",\"doi\":\"10.1016/j.chemgeo.2025.122756\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Calculation of the molar standard state Gibbs energies of aqueous ions, <span><math><msubsup><mi>G</mi><mn>2</mn><mi>o</mi></msubsup></math></span>, at supercritical temperatures and pressures is a prerequisite for thermodynamic modeling of hydrothermal processes. Currently, such calculation is performed only with the well-known HKF model, and the development of alternative methods is highly desirable to avoid any possible bias. As a step in this direction, the author presents a novel “isochoric” method for predicting the Gibbs energies of aqueous ions up to high temperatures and pressures. The method is based on the analysis of the temperature dependence of the partial molar isochoric heat capacity of aqueous ions, <span><math><msubsup><mi>C</mi><mrow><mi>v</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>. Knowing <span><math><msubsup><mi>C</mi><mrow><mi>v</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>, one can compute the partial molar isobaric heat capacity <span><math><msubsup><mi>C</mi><mrow><mi>p</mi><mo>,</mo><mn>2</mn></mrow><mi>o</mi></msubsup></math></span>, provided that <span><math><msubsup><mi>V</mi><mn>2</mn><mi>o</mi></msubsup></math></span> is known as a function of <em>T</em> and <em>P</em>. Then the calculation of <span><math><msubsup><mi>G</mi><mn>2</mn><mi>o</mi></msubsup></math></span> can be performed by the traditional methods. The test of this method was performed using two literature formulations (Arcis et al., 2024; Marshall and Franck, 1981) for the ionization constant of water over wide ranges of temperature (273–1273 K) and water density ρ (up to ρ = 1.25 g cm<sup>−3</sup>), which allow computing all thermodynamic properties of a hypothetical HOH electrolyte. Using 4 parameters at most, it is possible to reproduce the water ionization constants recommended by either Arcis et al. (2024) or Marshall and Franck (1981) formulations at supercritical temperatures with deviations less than those of these formulations. It is expected that the proposed “isochoric” method deserves further investigation.</div></div>\",\"PeriodicalId\":9847,\"journal\":{\"name\":\"Chemical Geology\",\"volume\":\"682 \",\"pages\":\"Article 122756\"},\"PeriodicalIF\":3.6000,\"publicationDate\":\"2025-03-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemical Geology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0009254125001469\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0009254125001469","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

摘要

计算超临界温度和压力下水溶液离子G2o的摩尔标准态吉布斯能是水热过程热力学建模的先决条件。目前,这样的计算只能用众所周知的HKF模型进行,而开发替代方法是非常必要的,以避免任何可能的偏差。作为朝这个方向迈出的一步,作者提出了一种新的“等共线”方法来预测高温高压下水溶液离子的吉布斯能。该方法是基于水离子的部分摩尔等时热容Cv, 20的温度依赖性分析。已知Cv, 20,就可以计算出偏摩尔等压热容Cp, 20,只要已知V2o是T和p的函数,那么G2o的计算就可以用传统的方法进行。采用两种文献公式对该方法进行检验(Arcis et al., 2024;Marshall和Franck, 1981)的电离常数的水在宽范围内的温度(273-1273 K)和水的密度ρ(高达ρ = 1.25 g cm−3),这允许计算所有的热力学性质的假设HOH电解质。最多使用4个参数,就有可能在超临界温度下重现Arcis等人(2024)或Marshall和Franck(1981)公式所推荐的水电离常数,其偏差小于这些公式。期望所提出的“等时线”方法值得进一步研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A novel method for correlating/predicting the thermodynamic properties of aqueous ions at high T and P
Calculation of the molar standard state Gibbs energies of aqueous ions, G2o, at supercritical temperatures and pressures is a prerequisite for thermodynamic modeling of hydrothermal processes. Currently, such calculation is performed only with the well-known HKF model, and the development of alternative methods is highly desirable to avoid any possible bias. As a step in this direction, the author presents a novel “isochoric” method for predicting the Gibbs energies of aqueous ions up to high temperatures and pressures. The method is based on the analysis of the temperature dependence of the partial molar isochoric heat capacity of aqueous ions, Cv,2o. Knowing Cv,2o, one can compute the partial molar isobaric heat capacity Cp,2o, provided that V2o is known as a function of T and P. Then the calculation of G2o can be performed by the traditional methods. The test of this method was performed using two literature formulations (Arcis et al., 2024; Marshall and Franck, 1981) for the ionization constant of water over wide ranges of temperature (273–1273 K) and water density ρ (up to ρ = 1.25 g cm−3), which allow computing all thermodynamic properties of a hypothetical HOH electrolyte. Using 4 parameters at most, it is possible to reproduce the water ionization constants recommended by either Arcis et al. (2024) or Marshall and Franck (1981) formulations at supercritical temperatures with deviations less than those of these formulations. It is expected that the proposed “isochoric” method deserves further investigation.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信