Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling

Although vanadinite (Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl) occurs in abundance in various terrestrial geochemical systems of natural and anthropogenic origin and is seriously considered as a potential nuclear waste sequestering agent, its actual applicatio...

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Main Authors: Justyna Topolska, Bartosz Puzio, Olaf Borkiewicz, Julia Sordyl, Maciej Manecki
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/2/135
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author Justyna Topolska
Bartosz Puzio
Olaf Borkiewicz
Julia Sordyl
Maciej Manecki
author_facet Justyna Topolska
Bartosz Puzio
Olaf Borkiewicz
Julia Sordyl
Maciej Manecki
author_sort Justyna Topolska
collection DOAJ
description Although vanadinite (Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl) occurs in abundance in various terrestrial geochemical systems of natural and anthropogenic origin and is seriously considered as a potential nuclear waste sequestering agent, its actual application is severely limited by a lack of understanding of its basic thermodynamic parameters. In this regard, the greatest challenge is posed by its incongruent dissolution, which is a pivotal hurdle for effective geochemical modeling. Our paper presents an universal approach for geochemical computing of systems undergoing incongruent dissolution which, along with unique, long-term experiments on vanadinites’ stability, allowed us to determine the mineral solubility constant. The dissolution experiments were carried out at pH = 3.5 for 12 years. Vanadinite has dissolved incongruently, continuously re-precipitating into chervetite (Pb<sub>2</sub>V<sub>2</sub>O<sub>7</sub>) with the two minerals remaining in mutual equilibrium until termination of the experiments. The empirically derived solubility constant K<sub>sp,V,298</sub> = 10<sup>–91.89 ± 0.05</sup> of vanadinite was determined for the first time. The proposed modeling method is versatile and can be adopted to other mineral systems undergoing incongruent dissolution.
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spelling doaj.art-cea4a22d59444e95ab11246e014b2b2a2023-12-03T15:12:58ZengMDPI AGMinerals2075-163X2021-01-0111213510.3390/min11020135Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution ModelingJustyna Topolska0Bartosz Puzio1Olaf Borkiewicz2Julia Sordyl3Maciej Manecki4Department of Mineralogy, Petrography and Geochemistry, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Kraków, PolandDepartment of Mineralogy, Petrography and Geochemistry, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Kraków, PolandX-ray Science Division, Advanced Photon Source, Argonne National Laboratory, 9700 South Cass Avenue, Bldg. 433, Argonne, IL 60439-4858, USADepartment of Mineralogy, Petrography and Geochemistry, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Kraków, PolandDepartment of Mineralogy, Petrography and Geochemistry, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Kraków, PolandAlthough vanadinite (Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl) occurs in abundance in various terrestrial geochemical systems of natural and anthropogenic origin and is seriously considered as a potential nuclear waste sequestering agent, its actual application is severely limited by a lack of understanding of its basic thermodynamic parameters. In this regard, the greatest challenge is posed by its incongruent dissolution, which is a pivotal hurdle for effective geochemical modeling. Our paper presents an universal approach for geochemical computing of systems undergoing incongruent dissolution which, along with unique, long-term experiments on vanadinites’ stability, allowed us to determine the mineral solubility constant. The dissolution experiments were carried out at pH = 3.5 for 12 years. Vanadinite has dissolved incongruently, continuously re-precipitating into chervetite (Pb<sub>2</sub>V<sub>2</sub>O<sub>7</sub>) with the two minerals remaining in mutual equilibrium until termination of the experiments. The empirically derived solubility constant K<sub>sp,V,298</sub> = 10<sup>–91.89 ± 0.05</sup> of vanadinite was determined for the first time. The proposed modeling method is versatile and can be adopted to other mineral systems undergoing incongruent dissolution.https://www.mdpi.com/2075-163X/11/2/135lead apatitechervetitesolubility productdissolution experimentthermodynamicsgeochemical modeling
spellingShingle Justyna Topolska
Bartosz Puzio
Olaf Borkiewicz
Julia Sordyl
Maciej Manecki
Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
Minerals
lead apatite
chervetite
solubility product
dissolution experiment
thermodynamics
geochemical modeling
title Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
title_full Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
title_fullStr Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
title_full_unstemmed Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
title_short Solubility Product of Vanadinite Pb<sub>5</sub>(VO<sub>4</sub>)<sub>3</sub>Cl at 25 °C—A Comprehensive Approach to Incongruent Dissolution Modeling
title_sort solubility product of vanadinite pb sub 5 sub vo sub 4 sub sub 3 sub cl at 25 °c a comprehensive approach to incongruent dissolution modeling
topic lead apatite
chervetite
solubility product
dissolution experiment
thermodynamics
geochemical modeling
url https://www.mdpi.com/2075-163X/11/2/135
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