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Coprecipitation of Ce with lead phosphates
AGH Univ Krakow, Dept Mineral Petrog & Geochem, Al Mickiewicza 30, PL-30059 Krakow, Poland..
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Earth Sciences, Mineralogy Petrology and Tectonics. AGH Univ Krakow, Dept Mineral Petrog & Geochem, Al Mickiewicza 30, PL-30059 Krakow, Poland..ORCID iD: 0000-0002-5772-5200
AGH Univ Krakow, Dept Mineral Petrog & Geochem, Al Mickiewicza 30, PL-30059 Krakow, Poland..
AGH Univ Krakow, Dept Mineral Petrog & Geochem, Al Mickiewicza 30, PL-30059 Krakow, Poland..
2025 (English)In: Chemie der Erde, ISSN 0009-2819, E-ISSN 1611-5864, Vol. 85, no 1, article id 126252Article in journal (Refereed) Published
Abstract [en]

Current development of sustainable technologies creates a demand for new sources of Rare Earth Elements (REE). Recent studies suggest that coprecipitation in the form of Pb-phosphates is one of the most effective methods in REE removal from aqueous solutions. This work focuses on the experimental study of the mechanisms of Ce coprecipitation with Pb phosphates, in particular with lead apatite - pyromorphite (Pb-5(PO4)(3)Cl). Coprecipitation experiments were conducted at ambient conditions, at pH range 1-11, by mixing solutions containing high concentrations of Pb and Ce (similar to 66,700 ppm and similar to 7600 ppm, respectively) with solutions containing stoichiometric concentrations of PO4 and Cl. As a result of coprecipitation with Pb phosphates, the Ce concentration decreased significantly to <2 ppm. The main product of the coprecipitation was Ce-doped pyromorphite (PymCe). Removal of Ce was most effective under alkaline conditions, while performance was slightly worse under acidic conditions, due in part to the slightly higher solubility of the precipitate. This was compared with a series of control experiments in the absence of either Pb, Cl, or Ce. Precipitation in the absence of Pb resulted in the formation of fibrous rhabdophane-Ce. In the absence of Cl, various phases were formed depending on pH conditions, such as 'phosphoschultenite' (PbHPO4), Pb-hopeite (PbPb2(PO4)(2)<middle dot>nH(2)O), mixed Pb and Ce hydrous phosphates, and hydroxylpyromorphite (Pb-5(PO4)(3)OH). In the absence of Ce, pure microcrystalline pyromorphite precipitated. Coprecipitation of Ce with Pb phosphates in the presence of Cl is advantageous due to the recovery of almost all Ce from solution in the form of a micro-crystalline Pym-Ce that is a very stable, insoluble phase easily separated from suspension. The precipitation of Pym-Ce is homogenous over a wide range of pH, assuring consistency in the obtained phases regardless of starting conditions. Achieved high Ce removal levels may be crucial for the progress of the REE extraction industry, in terms of this method being applicable to other REE for their recovery from solutions, including apatite leachates.

Place, publisher, year, edition, pages
Elsevier, 2025. Vol. 85, no 1, article id 126252
Keywords [en]
Rare earth elements, Pyromorphite, Pb-apatite, Apatite leaching, REE beneficiation
National Category
Physical Chemistry
Identifiers
URN: urn:nbn:se:uu:diva-553170DOI: 10.1016/j.chemer.2025.126252ISI: 001441736100001Scopus ID: 2-s2.0-85215863224OAI: oai:DiVA.org:uu-553170DiVA, id: diva2:1947638
Available from: 2025-03-26 Created: 2025-03-26 Last updated: 2025-03-26Bibliographically approved

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