Hydrothermal synthesis of α-Zn 2 SiO 4 :V phosphor, determination of oxidation states and structural localization of vanadium ions

2017 ◽  
Vol 87 ◽  
pp. 27-33 ◽  
Author(s):  
Rina F. Samigullina ◽  
Аlexander P. Tyutyunnik ◽  
Irina N. Gracheva ◽  
Тatiana I. Krasnenko ◽  
Natalia A. Zaitseva ◽  
...  
2009 ◽  
Vol 2009 (24) ◽  
pp. 3607-3612 ◽  
Author(s):  
Edurne S. Larrea ◽  
José L. Mesa ◽  
José L. Pizarro ◽  
Jesús Rodríguez-Fernández ◽  
María I. Arriortua ◽  
...  

2018 ◽  
Vol 73 (11) ◽  
pp. 803-811 ◽  
Author(s):  
Hagen Poddig ◽  
Jens Hunger ◽  
Sirko Kamusella ◽  
Hans-Henning Klauss ◽  
Thomas Doert

AbstractA new calcium iron ruthenium hydrogarnet with the approximate composition Ca3(Ru2−xFex)(FeO4)2−y(H4O4)1+y (x=1, y≈0.35) has been obtained by hydrothermal synthesis under oxidizing alkaline conditions. The compound crystallizes in the cubic space group Ia3̅d (No. 230) with a lattice parameter of a=12.4804(4) Å (T=100 K) and Z=8. The octahedral site of the garnet structure is equally occupied by Ru and Fe, whereas the tetrahedral site is partially occupied by Fe only. A partial substitution of the oxide anions by hydroxide ions is necessary for charge balancing, corresponding to the so-called hydrogarnet defects. The presence of hydroxide groups is proven by infrared spectroscopy. 57Fe Mössbauer spectroscopic data provide evidence for two different Fe3+ coordination environments as well as a magnetic ordering of two iron substructures with the respective ordering temperature above room temperature. The crystal composition was verified by energy-dispersive X-ray spectroscopy and the thermal behavior of the calcium iron ruthenate was studied by difference thermal analysis.


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