{"title":"Partial molar volumes of 1–1 electrolytes at high T and P: correlations and predictions","authors":"Andrey V. Plyasunov, Elena V. Cherkasova","doi":"10.1016/j.gca.2024.10.024","DOIUrl":null,"url":null,"abstract":"Knowledge of the partial molar volumes of aqueous ions allows accurate calculation of the pressure dependence of equilibrium constants, solubility of minerals, etc., thus being useful for thermodynamic modeling of hydrothermal processes. This study analyzed methods to correlate and predict the values of the partial molar volumes at infinite dilution, <mml:math altimg=\"si6.svg\"><mml:mrow><mml:msubsup><mml:mi>V</mml:mi><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mi mathvariant=\"normal\">o</mml:mi></mml:msubsup></mml:mrow></mml:math>, for 1–1 electrolytes and singly charged ions at elevated T and P. Since the precise experimental values of the dielectric constant of water are measured only up to 873 K, we were interested only in non-electrostatic ways to correlate <mml:math altimg=\"si6.svg\"><mml:mrow><mml:msubsup><mml:mi>V</mml:mi><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mi mathvariant=\"normal\">o</mml:mi></mml:msubsup></mml:mrow></mml:math> data. First of all, we compiled the <mml:math altimg=\"si6.svg\"><mml:mrow><mml:msubsup><mml:mi>V</mml:mi><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mi mathvariant=\"normal\">o</mml:mi></mml:msubsup></mml:mrow></mml:math> values at T > 373 K for the following 1–1 electrolytes: HCl, LiCl, LiI, LiNO<ce:inf loc=\"post\">3</ce:inf>, LiOH, NaF, NaCl, NaBr, NaI, NaNO<ce:inf loc=\"post\">3</ce:inf>, NaOH, NaHCO<ce:inf loc=\"post\">3</ce:inf>, NaClO<ce:inf loc=\"post\">4</ce:inf>, NaH<ce:inf loc=\"post\">2</ce:inf>PO<ce:inf loc=\"post\">4</ce:inf>, NaTr (Tr stands for triflate), KF, KCl, KBr, KI, KNO<ce:inf loc=\"post\">3</ce:inf>, KOH, CsBr, and NH<ce:inf loc=\"post\">4</ce:inf>Cl. Relations, following from the “density” model and from the Fluctuation Solution Theory (FST) were employed to analyze data. It was concluded that at the current state of knowledge of <mml:math altimg=\"si6.svg\"><mml:mrow><mml:msubsup><mml:mi>V</mml:mi><mml:mrow><mml:mn>2</mml:mn></mml:mrow><mml:mi mathvariant=\"normal\">o</mml:mi></mml:msubsup></mml:mrow></mml:math> the FST-relations for electrolytes are recommended mainly to reject strongly deviating experimental outliers. However, the “density” model provides a simple and fairly accurate way to describe the compiled set of data with only two parameters for each ion, <mml:math altimg=\"si4.svg\"><mml:mrow><mml:mi>n</mml:mi></mml:mrow></mml:math> and <mml:math altimg=\"si5.svg\"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>hc</mml:mtext></mml:msub></mml:mrow></mml:math>, values of which were evaluated for the following singly-charged ions: H<ce:sup loc=\"post\">+</ce:sup>, Li<ce:sup loc=\"post\">+</ce:sup>, Na<ce:sup loc=\"post\">+</ce:sup>, K<ce:sup loc=\"post\">+</ce:sup>, Cs<ce:sup loc=\"post\">+</ce:sup>, NH<ce:inf loc=\"post\">4</ce:inf><ce:sup loc=\"post\">+</ce:sup>, F<ce:sup loc=\"post\">-</ce:sup>, Cl<ce:sup loc=\"post\">-</ce:sup>, Br<ce:sup loc=\"post\">-</ce:sup>, I<ce:sup loc=\"post\">-</ce:sup>, OH<ce:sup loc=\"post\">–</ce:sup>, NO<ce:inf loc=\"post\">3</ce:inf><ce:sup loc=\"post\">–</ce:sup>, H<ce:inf loc=\"post\">2</ce:inf>PO<ce:inf loc=\"post\">4</ce:inf><ce:sup loc=\"post\">-</ce:sup>, HCO<ce:inf loc=\"post\">3</ce:inf><ce:sup loc=\"post\">–</ce:sup>, ClO<ce:inf loc=\"post\">4</ce:inf><ce:sup loc=\"post\">-</ce:sup>, Tr<ce:sup loc=\"post\">-</ce:sup> (Tr = triflate). Following <ce:cross-ref ref>Mesmer et al. (1988)</ce:cross-ref>, we consider the fitting parameters <mml:math altimg=\"si5.svg\"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>hc</mml:mtext></mml:msub></mml:mrow></mml:math> and <mml:math altimg=\"si4.svg\"><mml:mrow><mml:mi>n</mml:mi></mml:mrow></mml:math> to be related to the intrinsic volume of the ion and to the number of water molecules transferred from the bulk water to a hydration shell around the ion, respectively.","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"74 1","pages":""},"PeriodicalIF":4.5000,"publicationDate":"2024-10-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochimica et Cosmochimica Acta","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1016/j.gca.2024.10.024","RegionNum":1,"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
Abstract
Knowledge of the partial molar volumes of aqueous ions allows accurate calculation of the pressure dependence of equilibrium constants, solubility of minerals, etc., thus being useful for thermodynamic modeling of hydrothermal processes. This study analyzed methods to correlate and predict the values of the partial molar volumes at infinite dilution, V2o, for 1–1 electrolytes and singly charged ions at elevated T and P. Since the precise experimental values of the dielectric constant of water are measured only up to 873 K, we were interested only in non-electrostatic ways to correlate V2o data. First of all, we compiled the V2o values at T > 373 K for the following 1–1 electrolytes: HCl, LiCl, LiI, LiNO3, LiOH, NaF, NaCl, NaBr, NaI, NaNO3, NaOH, NaHCO3, NaClO4, NaH2PO4, NaTr (Tr stands for triflate), KF, KCl, KBr, KI, KNO3, KOH, CsBr, and NH4Cl. Relations, following from the “density” model and from the Fluctuation Solution Theory (FST) were employed to analyze data. It was concluded that at the current state of knowledge of V2o the FST-relations for electrolytes are recommended mainly to reject strongly deviating experimental outliers. However, the “density” model provides a simple and fairly accurate way to describe the compiled set of data with only two parameters for each ion, n and Vhc, values of which were evaluated for the following singly-charged ions: H+, Li+, Na+, K+, Cs+, NH4+, F-, Cl-, Br-, I-, OH–, NO3–, H2PO4-, HCO3–, ClO4-, Tr- (Tr = triflate). Following Mesmer et al. (1988), we consider the fitting parameters Vhc and n to be related to the intrinsic volume of the ion and to the number of water molecules transferred from the bulk water to a hydration shell around the ion, respectively.
期刊介绍:
Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes:
1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids
2). Igneous and metamorphic petrology
3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth
4). Organic geochemistry
5). Isotope geochemistry
6). Meteoritics and meteorite impacts
7). Lunar science; and
8). Planetary geochemistry.