{"title":"碳酸盐化合物与钠离子和钾离子相互作用的 SIT 模型参数说明了关联性","authors":"Andrey V. Plyasunov, Elena V. Cherkasova","doi":"10.1016/j.apgeochem.2024.106119","DOIUrl":null,"url":null,"abstract":"<div><p>The current study is devoted to the determination of the SIT coefficients at 298.15 K for interactions, involving <span><math><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub><mrow><mo>(</mo><mtext>aq</mtext><mo>)</mo></mrow></mrow></math></span>, <span><math><mrow><mtext>HC</mtext><msubsup><mi>O</mi><mn>3</mn><mo>−</mo></msubsup></mrow></math></span>, and <span><math><mrow><mi>C</mi><msubsup><mi>O</mi><mn>3</mn><mrow><mn>2</mn><mo>‐</mo></mrow></msubsup></mrow></math></span>, with mostly Na<sup>+</sup> and K<sup>+</sup> ions. The SIT model is a simple yet physically sound model for activity coefficients in aqueous solutions, that has just one parameter for each cation-anion or a dissolved gas – electrolyte interaction. Among the issues that were met for carbonate systems are the side reactions of hydrolysis and disproportionation in the carbonate solutions, that complicate the analysis of data and lead to unusually large difference, up to 9%, in the values of activity coefficients, determined in different authoritative laboratories. For <span><math><mrow><msub><mtext>Na</mtext><mn>2</mn></msub><mi>C</mi><msub><mi>O</mi><mn>3</mn></msub></mrow></math></span> and <span><math><mrow><msub><mi>K</mi><mn>2</mn></msub><mi>C</mi><msub><mi>O</mi><mn>3</mn></msub></mrow></math></span> solutions, it was necessary to take into account the reaction of formation of the ionic pair <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>+</mo><mi>C</mi><msubsup><mi>O</mi><mn>3</mn><mrow><mn>2</mn><mo>‐</mo></mrow></msubsup><mo>=</mo><mtext>MC</mtext><msubsup><mi>O</mi><mn>3</mn><mo>−</mo></msubsup></mrow></math></span>, with the equilibrium constants <span><math><mrow><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup></mrow></math></span> equal to <span><math><mrow><msub><mi>log</mi><mn>10</mn></msub><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup><mo>=</mo></mrow></math></span> 0.75 ± 0.08 for <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>=</mo><mi>N</mi><msup><mi>a</mi><mo>+</mo></msup></mrow></math></span> and to <span><math><mrow><msub><mi>log</mi><mn>10</mn></msub><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup><mo>=</mo></mrow></math></span> 0.67 ± 0.11 for <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>=</mo><msup><mi>K</mi><mo>+</mo></msup></mrow></math></span>. In all, there are values for more than 20 binary SIT interaction coefficients. All results are valid at 298.15 K, 0.1 MPa.</p></div>","PeriodicalId":8064,"journal":{"name":"Applied Geochemistry","volume":"172 ","pages":"Article 106119"},"PeriodicalIF":3.1000,"publicationDate":"2024-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The SIT model parameters for interactions of carbonate compounds with sodium and potassium ions accounting for association\",\"authors\":\"Andrey V. Plyasunov, Elena V. Cherkasova\",\"doi\":\"10.1016/j.apgeochem.2024.106119\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The current study is devoted to the determination of the SIT coefficients at 298.15 K for interactions, involving <span><math><mrow><mi>C</mi><msub><mi>O</mi><mn>2</mn></msub><mrow><mo>(</mo><mtext>aq</mtext><mo>)</mo></mrow></mrow></math></span>, <span><math><mrow><mtext>HC</mtext><msubsup><mi>O</mi><mn>3</mn><mo>−</mo></msubsup></mrow></math></span>, and <span><math><mrow><mi>C</mi><msubsup><mi>O</mi><mn>3</mn><mrow><mn>2</mn><mo>‐</mo></mrow></msubsup></mrow></math></span>, with mostly Na<sup>+</sup> and K<sup>+</sup> ions. The SIT model is a simple yet physically sound model for activity coefficients in aqueous solutions, that has just one parameter for each cation-anion or a dissolved gas – electrolyte interaction. Among the issues that were met for carbonate systems are the side reactions of hydrolysis and disproportionation in the carbonate solutions, that complicate the analysis of data and lead to unusually large difference, up to 9%, in the values of activity coefficients, determined in different authoritative laboratories. For <span><math><mrow><msub><mtext>Na</mtext><mn>2</mn></msub><mi>C</mi><msub><mi>O</mi><mn>3</mn></msub></mrow></math></span> and <span><math><mrow><msub><mi>K</mi><mn>2</mn></msub><mi>C</mi><msub><mi>O</mi><mn>3</mn></msub></mrow></math></span> solutions, it was necessary to take into account the reaction of formation of the ionic pair <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>+</mo><mi>C</mi><msubsup><mi>O</mi><mn>3</mn><mrow><mn>2</mn><mo>‐</mo></mrow></msubsup><mo>=</mo><mtext>MC</mtext><msubsup><mi>O</mi><mn>3</mn><mo>−</mo></msubsup></mrow></math></span>, with the equilibrium constants <span><math><mrow><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup></mrow></math></span> equal to <span><math><mrow><msub><mi>log</mi><mn>10</mn></msub><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup><mo>=</mo></mrow></math></span> 0.75 ± 0.08 for <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>=</mo><mi>N</mi><msup><mi>a</mi><mo>+</mo></msup></mrow></math></span> and to <span><math><mrow><msub><mi>log</mi><mn>10</mn></msub><msubsup><mi>β</mi><mn>1</mn><mi>o</mi></msubsup><mo>=</mo></mrow></math></span> 0.67 ± 0.11 for <span><math><mrow><msup><mi>M</mi><mo>+</mo></msup><mo>=</mo><msup><mi>K</mi><mo>+</mo></msup></mrow></math></span>. In all, there are values for more than 20 binary SIT interaction coefficients. All results are valid at 298.15 K, 0.1 MPa.</p></div>\",\"PeriodicalId\":8064,\"journal\":{\"name\":\"Applied Geochemistry\",\"volume\":\"172 \",\"pages\":\"Article 106119\"},\"PeriodicalIF\":3.1000,\"publicationDate\":\"2024-07-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Geochemistry\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0883292724002245\",\"RegionNum\":3,\"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":"Applied Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0883292724002245","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
The SIT model parameters for interactions of carbonate compounds with sodium and potassium ions accounting for association
The current study is devoted to the determination of the SIT coefficients at 298.15 K for interactions, involving , , and , with mostly Na+ and K+ ions. The SIT model is a simple yet physically sound model for activity coefficients in aqueous solutions, that has just one parameter for each cation-anion or a dissolved gas – electrolyte interaction. Among the issues that were met for carbonate systems are the side reactions of hydrolysis and disproportionation in the carbonate solutions, that complicate the analysis of data and lead to unusually large difference, up to 9%, in the values of activity coefficients, determined in different authoritative laboratories. For and solutions, it was necessary to take into account the reaction of formation of the ionic pair , with the equilibrium constants equal to 0.75 ± 0.08 for and to 0.67 ± 0.11 for . In all, there are values for more than 20 binary SIT interaction coefficients. All results are valid at 298.15 K, 0.1 MPa.
期刊介绍:
Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application.
Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.