Formation of Noble Metal Phases (Pt, Pd, Rh, Ru, Ir, Au, Ag) in the Process of Fractional Crystallization of the CuFeS2 Melt

Formation of Noble Metal Phases (Pt, Pd, Rh, Ru, Ir, Au, Ag) in the Process of Fractional Crystallization of the CuFeS2 Melt Научная публикация

Журнал

Minerals
ISSN: 2075-163X

Вых. Данные

Год: 2022, Том: 12, Номер: 9, Номер статьи : 1136, Страниц : 19 DOI: 10.3390/min12091136

Ключевые слова

Cu-Fe-S system; noble metals; directional crystallization; intermediate solid solution; fine inclusions

Авторы

Sinyakova Elena Fedorovna ¹ , Vasilyeva Inga Grigorievna ² , Oreshonkov Aleksandr Sergeevich ^3,4 , Goryainov Sergey Vladimirovich ¹ , Karmanov Nikolay Semenovich ¹

Организации

1	V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, 630090 Novosibirsk, Russia
2	Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the Russian Academy of Sciences, Ac. Lavrentieva ave. 3, 630090 Novosibirsk, Russia
3	Laboratory of Molecular Spectroscopy, Kirensky Institute of Physics, Federal Research Center KSC SB RAS, Akademgorodok 50/38, 660036 Krasnoyarsk, Russia
4	School of Engineering and Construction, Siberian Federal University, 660041 Krasnoyarsk, Russia

The quasi-equilibrium directional crystallization of the melt composition (at. %): Cu 24.998, Fe 25.001, S 49.983, with Ag 0.002, Pd 0.003, Ru 0.004, Rh 0.006, and Au, Pt, Ir (each as 0.001) was carried out. The crystallized cylindrical ingot consisted of two primary zones and three secondary zones with different chemical and phase compositions. The compositions of the primary zones corresponded to high-temperature intermediate solid solution (zone I) and liquid enriched in sulfur (zone II). The compositions of the secondary zones corresponded to low-temperature intermediate solid solution and chalcopyrite (zone Ia), the same intermediate solid solution with chalcopyrite and bornite (zone Ib), and again with bornite, chalcocite, and idaite (zone II). We plotted the distribution curves of Fe, Cu, and S along the ingot, calculated the distribution coefficients of the components during directional crystallization, and clearly showed that, from the initial stoichiometric composition CuFeS2, the intermediate solid solution enriched in Fe and depleted in S is crystallized. Based on the data of directional crystallization and thermal analysis, a cross section was constructed in the intermediate solid solution-sulfide melt region of the Cu-Fe-S system. With solubility in the solid Cu-Fe sulfides lying below detection limit of scanning electron microscopy/energy-dispersive X-ray spectrometry (SEM/EDS), noble elements occurred as individual phases of a size more often <10 µm. They were identified as Ag, RuS2, PdS, Au* (an Au based alloy), (Rh, Ir, Ru)3S8, (Rh, Ir)3S8, Rh3S8, and (Cu, Fe)~2(Pt, Rh)1S~5 phases by electron microprobe. Based on ab initio calculations of crystal structure, electronic band structure, and lattice dynamics of idealized laurite RuS2 phase and the idealized Ir3S8, Rh3S8, and Ru3S8 phases, the interpretation of Raman spectrum of the cation-mixed (Ru, Rh, Ir)S2 sulfide was presented for the first time.

Sinyakova E.F. , Vasilyeva I.G. , Oreshonkov A.S. , Goryainov S.V. , Karmanov N.S.
Formation of Noble Metal Phases (Pt, Pd, Rh, Ru, Ir, Au, Ag) in the Process of Fractional Crystallization of the CuFeS2 Melt
Minerals. 2022. V.12. N9. 1136 :1-19. DOI: 10.3390/min12091136 WOS Scopus OpenAlex

Поступила в редакцию:	6 авг. 2022 г.
Принята к публикации:	2 сент. 2022 г.
Опубликована в печати:	7 сент. 2022 г.
Опубликована online:	7 сент. 2022 г.

Web of science:	WOS:000859687200001
Scopus:	2-s2.0-85138709665
OpenAlex:	W4295008038

БД	Цитирований
Web of science	10
Scopus	9
OpenAlex	9