Y. Yan, N. Çevirim-Papaioannou, X. Gaona, D. Fellhauer, M. Altmaier
{"title":"氯化物体系中 U(IV)溶解和水解的热力学描述:U4+-Na+-Mg2+-Ca2+-H+-Cl--OH--H2O(l) 体系的皮策活性模型","authors":"Y. Yan, N. Çevirim-Papaioannou, X. Gaona, D. Fellhauer, M. Altmaier","doi":"10.1016/j.apgeochem.2024.106091","DOIUrl":null,"url":null,"abstract":"<div><p>This study presents updated chemical, thermodynamic, and activity models for the system U<sup>4+</sup>–Na<sup>+</sup>–Mg<sup>2+</sup>–Ca<sup>2+</sup>–H<sup>+</sup>–Cl<sup>–</sup>–OH<sup>–</sup>–H<sub>2</sub>O(l) derived using the Pitzer formalism and a strict ion interaction approach. The models build on comprehensive solubility datasets in dilute to concentrated NaCl, MgCl<sub>2</sub>, and CaCl<sub>2</sub> solutions. The Nuclear Energy Agency-Thermochemical Database (NEA-TDB) selection of solubility and hydrolysis constants in the reference state were taken as anchoring point, and were extended further with the solid nanocrystalline phase UO<sub>2</sub>∙H<sub>2</sub>O(ncr) and the ternary complex Ca<sub>4</sub> [U(OH)<sub>8</sub>]<sup>4+</sup>. The former was identified in long-term solubility experiments at ambient conditions, whereas the latter has been selected in analogy to Th(IV), Np(IV), and Pu(IV) considering experimental evidences available for these An(IV) in alkaline, concentrated CaCl<sub>2</sub> solutions. These models represent an improved tool for the calculation of U(IV) solubility and aqueous speciation in a variety of geochemical conditions including concentrated brine systems relevant in salt-based repositories for nuclear waste disposal.</p></div>","PeriodicalId":8064,"journal":{"name":"Applied Geochemistry","volume":"171 ","pages":"Article 106091"},"PeriodicalIF":3.1000,"publicationDate":"2024-07-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0883292724001963/pdfft?md5=9cac09ae1b98feced0cdce8502e75c5e&pid=1-s2.0-S0883292724001963-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Thermodynamic description of U(IV) solubility and hydrolysis in chloride systems: Pitzer activity model for the system U4+–Na+–Mg2+–Ca2+–H+–Cl––OH––H2O(l)\",\"authors\":\"Y. Yan, N. Çevirim-Papaioannou, X. Gaona, D. Fellhauer, M. Altmaier\",\"doi\":\"10.1016/j.apgeochem.2024.106091\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>This study presents updated chemical, thermodynamic, and activity models for the system U<sup>4+</sup>–Na<sup>+</sup>–Mg<sup>2+</sup>–Ca<sup>2+</sup>–H<sup>+</sup>–Cl<sup>–</sup>–OH<sup>–</sup>–H<sub>2</sub>O(l) derived using the Pitzer formalism and a strict ion interaction approach. The models build on comprehensive solubility datasets in dilute to concentrated NaCl, MgCl<sub>2</sub>, and CaCl<sub>2</sub> solutions. The Nuclear Energy Agency-Thermochemical Database (NEA-TDB) selection of solubility and hydrolysis constants in the reference state were taken as anchoring point, and were extended further with the solid nanocrystalline phase UO<sub>2</sub>∙H<sub>2</sub>O(ncr) and the ternary complex Ca<sub>4</sub> [U(OH)<sub>8</sub>]<sup>4+</sup>. The former was identified in long-term solubility experiments at ambient conditions, whereas the latter has been selected in analogy to Th(IV), Np(IV), and Pu(IV) considering experimental evidences available for these An(IV) in alkaline, concentrated CaCl<sub>2</sub> solutions. These models represent an improved tool for the calculation of U(IV) solubility and aqueous speciation in a variety of geochemical conditions including concentrated brine systems relevant in salt-based repositories for nuclear waste disposal.</p></div>\",\"PeriodicalId\":8064,\"journal\":{\"name\":\"Applied Geochemistry\",\"volume\":\"171 \",\"pages\":\"Article 106091\"},\"PeriodicalIF\":3.1000,\"publicationDate\":\"2024-07-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S0883292724001963/pdfft?md5=9cac09ae1b98feced0cdce8502e75c5e&pid=1-s2.0-S0883292724001963-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Geochemistry\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0883292724001963\",\"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/S0883292724001963","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}
Thermodynamic description of U(IV) solubility and hydrolysis in chloride systems: Pitzer activity model for the system U4+–Na+–Mg2+–Ca2+–H+–Cl––OH––H2O(l)
This study presents updated chemical, thermodynamic, and activity models for the system U4+–Na+–Mg2+–Ca2+–H+–Cl––OH––H2O(l) derived using the Pitzer formalism and a strict ion interaction approach. The models build on comprehensive solubility datasets in dilute to concentrated NaCl, MgCl2, and CaCl2 solutions. The Nuclear Energy Agency-Thermochemical Database (NEA-TDB) selection of solubility and hydrolysis constants in the reference state were taken as anchoring point, and were extended further with the solid nanocrystalline phase UO2∙H2O(ncr) and the ternary complex Ca4 [U(OH)8]4+. The former was identified in long-term solubility experiments at ambient conditions, whereas the latter has been selected in analogy to Th(IV), Np(IV), and Pu(IV) considering experimental evidences available for these An(IV) in alkaline, concentrated CaCl2 solutions. These models represent an improved tool for the calculation of U(IV) solubility and aqueous speciation in a variety of geochemical conditions including concentrated brine systems relevant in salt-based repositories for nuclear waste disposal.
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.