Extending the mineralogy of U <sup>6+</sup> (I): Crystal structure of lepersonnite-(Gd) and a description of the new mineral lepersonnite-(Nd)

Abstract Two uranyl carbonate silicate minerals have been studied in detail, lepersonnite-(Gd) and the new mineral lepersonnite-(Nd). Both minerals originate from Katanga province in the Democratic Republic of Congo (Africa): lepersonnite-(Gd) from the Shinkolobwe mine (type locality) and lepersonnite-(Nd) from the Swambo mine (type locality) and Shinkolobwe mine. Each occurs as radial to acicular aggregates composed of long prismatic, thin crystals, as the products of hydration–oxidation weathering of uraninite. A detailed description of the chemical and physical properties of lepersonnite-(Nd) is provided, including the thermal analysis of the -(Gd) member. Moreover, Raman and infrared spectroscopy data are provided for both minerals. The crystal structure of lepersonnite-(Gd) has been solved based on 3D electron diffraction data. According to the best dataset at 95 K, lepersonnite-(Gd) is orthorhombic, with a = 11.838(134) Å, b = 15.822(333) Å, c = 39.147(190) Å and V = 7353(282) Å 3 ( Z = 4). The dynamic refinement of the crystal structure ( R obs / wR obs = 0.1204/0.1088 and R all / wR all = 0.1204/0.1088 for 3090/50507 observed/all reflections and 247 refined parameters) revealed a large complex sheet structure with structural units defining a new lepersonnite topology. It contains infinite sheets of uranyl polyhedra, planar CO 3 groups, protonated Si-tetrahedra, and Gd 3+ polyhedra, and a thick interlayer hosted with H 2 O and partially occupied Ca 2+ sites. Based on the structure refinement, bond-valence considerations, and new electron microprobe data, we infer that the ideal formula of lepersonnite-(Gd) is [Ca 0.5 Gd 0.5 (H 2 O) 18 (OH) 1.5 ] [Gd(UO 2 ) 12 (SiO 3 OH) 2 (CO 3 ) 4 (OH) 10 O 2 (H 2 O) 5 ]. On the basis of their closely related powder X-ray diffraction patterns and the similar behaviour of Nd and Gd, we expect the two minerals to adopt the same structures, apart from Ca, which was absent in lepersonnite-(Nd). The ideal formula for lepersonnite-(Nd) is [Nd(H 2 O) 18 (OH) 2 ][Nd(UO 2 ) 12 (SiO 3 OH) 2 (CO 3 ) 4 (OH) 10 O 2 (H 2 O) 5 ].

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Publication Details

Journal
Mineralogical Magazine
Published
2025-07-14
DOI
https://doi.org/10.1180/mgm.2025.29
Citations
2
Primary Topic
Radioactive element chemistry and processing
Type
article
Field-Weighted Citation Impact
1.07

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article

Extending the mineralogy of U 6+ (I): Crystal structure of lepersonnite-(Gd) and a description of the new mineral lepersonnite-(Nd)

Jiří Sejkora, Radek Škoda, Nicolas Meisser, Simon Philippo et al.
2 citations
Mineralogical Magazine
Radioactive element chemistry and processing
1.07
article

Extending the mineralogy of U 6+ (I): Crystal structure of lepersonnite-(Gd) and a description of the new mineral lepersonnite-(Nd)

Jiří Sejkora, Radek Škoda, Nicolas Meisser, Simon Philippo, Zdeněk Dolníček, Jakub Plášil, Gwladys Steciuk, Jan Robin Rohlicek, Martin Ondrejka, Maël Guennou, Florias Mees, Pavel Uher, A. R. Kampf
article en
2 citations

Abstract

Abstract Two uranyl carbonate silicate minerals have been studied in detail, lepersonnite-(Gd) and the new mineral lepersonnite-(Nd). Both minerals originate from Katanga province in the Democratic Republic of Congo (Africa): lepersonnite-(Gd) from the Shinkolobwe mine (type locality) and lepersonnite-(Nd) from the Swambo mine (type locality) and Shinkolobwe mine. Each occurs as radial to acicular aggregates composed of long prismatic, thin crystals, as the products of hydration–oxidation weathering of uraninite. A detailed description of the chemical and physical properties of lepersonnite-(Nd) is provided, including the thermal analysis of the -(Gd) member. Moreover, Raman and infrared spectroscopy data are provided for both minerals. The crystal structure of lepersonnite-(Gd) has been solved based on 3D electron diffraction data. According to the best dataset at 95 K, lepersonnite-(Gd) is orthorhombic, with a = 11.838(134) Å, b = 15.822(333) Å, c = 39.147(190) Å and V = 7353(282) Å 3 ( Z = 4). The dynamic refinement of the crystal structure ( R obs / wR obs = 0.1204/0.1088 and R all / wR all = 0.1204/0.1088 for 3090/50507 observed/all reflections and 247 refined parameters) revealed a large complex sheet structure with structural units defining a new lepersonnite topology. It contains infinite sheets of uranyl polyhedra, planar CO 3 groups, protonated Si-tetrahedra, and Gd 3+ polyhedra, and a thick interlayer hosted with H 2 O and partially occupied Ca 2+ sites. Based on the structure refinement, bond-valence considerations, and new electron microprobe data, we infer that the ideal formula of lepersonnite-(Gd) is [Ca 0.5 Gd 0.5 (H 2 O) 18 (OH) 1.5 ] [Gd(UO 2 ) 12 (SiO 3 OH) 2 (CO 3 ) 4 (OH) 10 O 2 (H 2 O) 5 ]. On the basis of their closely related powder X-ray diffraction patterns and the similar behaviour of Nd and Gd, we expect the two minerals to adopt the same structures, apart from Ca, which was absent in lepersonnite-(Nd). The ideal formula for lepersonnite-(Nd) is [Nd(H 2 O) 18 (OH) 2 ][Nd(UO 2 ) 12 (SiO 3 OH) 2 (CO 3 ) 4 (OH) 10 O 2 (H 2 O) 5 ].

Mineralogical MagazineVol. 89(5)
Royal Museum for Central Africa (BE), University of Luxembourg (LU), Masaryk University (CZ), Perot Museum of Nature and Science (US), Natural History Museum of Los Angeles County (US), FZU ‒ Institute of Physics of the Academy of Sciences of the Czech Republic (CZ), Musée national d'histoire naturelle Luxembourg (LU), Comenius University Bratislava (SK)
Ministerstvo Školství, Mládeže a Tělovýchovy, Vysoká Škola Chemicko-technologická v Praze
Openalex Percentile: Top 22%
Radioactive element chemistry and processing
1.07
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