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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Phase relations in the Bi$_2$O$_3$–Mn$_2$O$_3$–M$_2$O$_3$ (M=Fe, Al, and Ga) pseudoternary systems</dc:title><dc:creator>Škapin,	Srečo D.	(Avtor)
	</dc:creator><dc:creator>Golobič,	Amalija	(Avtor)
	</dc:creator><dc:creator>Spreitzer,	Matjaž	(Avtor)
	</dc:creator><dc:creator>Suvorov,	Danilo	(Avtor)
	</dc:creator><dc:subject>electronic ceramics</dc:subject><dc:subject>phase relations</dc:subject><dc:subject>phase diagram</dc:subject><dc:subject>high-temperature phase relations</dc:subject><dc:subject>ternary systems Bi$_2$O$_3$–Mn$_2$O$_3$–M$_2$O$_3$ (M=Fe</dc:subject><dc:subject>Ga</dc:subject><dc:subject>Al)</dc:subject><dc:description>This study establishes the subsolidus phase relations in the Bi$_2$O$_3$–Mn$_2$O$_3$–M$_2$O$_3$ (M = Fe, Al, and Ga) systems at 770°C in an oxidizing air environment, with a specific focus on identifying of phase stability and extension of solid solubility of new solid solutions. The pseudoternary nature of these systems is influenced by the presence of both Mn$^{3+}$ and Mn$^{4+}$ oxidation states in mullite Bi$_2$Mn$_4$O$_{10}$-based phases and Mn$^{4+}$ in sillenite Bi$_{12}$MnO$_{20}$-based phases. Our findings reveal that the addition of M$_2$O$_3$ (where M = Fe, Al, and Ga) in small amounts (up to 1.5 mol%) to Bi$_2$O$_3$ promotes the formation of the γ-Bi$_2$O$_3$ phase. However, with increased M$_2$O$_3$ addition (up to 7 mol%), isomorphous sillenite compounds Bi$_{25}$MO$_{39}$ are formed. These findings clearly show differences between the two phases, γ-Bi$_2$O$_3$ and sillenite Bi$_{25}$MO$_{39}$ which have been largely incorrectly defined in the past. In contrast, in the binary system Bi$_2$O$_3$–Mn$_2$O$_3$ the γ-Bi$_2$O$_3$ was not identified. The sillenite compounds Bi$_{12}$MnO$_{20}$ and Bi$_{25}$MO$_{39}$ exhibit solid solubility in all three systems M = Fe, Al, and Ga over the entire composition range. Additionally, the perovskite phase BiFeO$_3$ exhibits an extended solid solubility, incorporating up to 32 at% of Mn as a substitution for Fe however the perovskite-type BiGaO$_3$ and BiAlO$_3$ were not confirmed in the investigated systems. In the investigated systems, the mullite-type Bi$_2$Mn$_4$O$_{10}$ and Bi$_2$M$_4$O$_9$ (M = Fe, Al, and Ga) form solid solutions with various compositional extensions, which depends on the difference of ionic size of M atoms (Fe, Al, and Ga) in comparison of Mn size. Based on experimental results, the three phase diagrams of the Bi$_2$O$_3$–Mn$_2$O$_3$–M$_2$O$_3$ (M = Fe, Al, and Ga) systems were constructed. </dc:description><dc:date>2025</dc:date><dc:date>2025-03-05 15:05:31</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>167664</dc:identifier><dc:identifier>UDK: 54</dc:identifier><dc:identifier>ISSN pri članku: 1551-2916</dc:identifier><dc:identifier>DOI: 10.1111/jace.20323</dc:identifier><dc:identifier>COBISS_ID: 224011011</dc:identifier><dc:language>sl</dc:language></metadata>
