首页> 外文期刊>Journal of Advanced Ceramics >Structural, vibrational and magnetic properties of Ti substituted bulk hematite: Emphasis Type="Italic"α/Emphasis-FeSubscript2?Emphasis Type="Italic"x/Emphasis/SubscriptTiSubscript Emphasis Type="Italic"x/Emphasis /SubscriptOSubscript3/Subscript
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Structural, vibrational and magnetic properties of Ti substituted bulk hematite: Emphasis Type="Italic"α/Emphasis-FeSubscript2?Emphasis Type="Italic"x/Emphasis/SubscriptTiSubscript Emphasis Type="Italic"x/Emphasis /SubscriptOSubscript3/Subscript

机译:Ti取代的块状赤铁矿的结构,振动和磁性:α -Fe 2? x Ti x O 3

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Ti doped hematite α-Fe2?xTixO3 (x = 0.0, 0.0206 and 0.0344) samples are synthesized using solid-state ceramic route technique. Single phase and corundum (Al2O3) type structure is revealed from the X-ray diffraction (XRD) pattern. On substitution of Ti at Fe site, all Raman active modes are shifted to higher wave numbers. An additional feature of Eu (LO) mode at about 660 cm-1 is observed. The Eu mode frequency is decreased and pronounced systematically as a function of Ti doping, and it reaches a value of 658 cm?1 for x = 0.0344. The coercivity Hc (remanence Mr) for x = 0.0, 0.0206 and 0.0344 are determined to be 995 Oe (0.44 emu/mg), 1404 Oe (0.00019 emu/mg) and 2023 Oe (0.00016 emu/mg), respectively. The larger coercivity for Ti doped samples can be attributed to their enhanced shape and magneto-crystalline anisotropy. The observed isomer shift (δ) from room temperature M?ssbauer data clearly shows the presence of ferric (Fe3+) and Ti4+ ions illustrating strong ferromagnetic ordering up to x = 0.0206 in α-Fe2?xTixO3 hematite and weak ferromagnetic ordering of α-Fe2?xTixO3 for x = 0.0344.
机译:使用固态陶瓷路线技术合成了掺钛的赤铁矿α-Fe2αxTixO3(x = 0.0、0.0206和0.0344)样品。从X射线衍射(XRD)图可以看出单相和刚玉(Al2O3)型结构。在Fe处置换Ti后,所有拉曼激活模式都转移到更高的波数上。在大约660 cm-1处观察到Eu(LO)模式的另一个特征。 Eu模式频率根据Ti掺杂而系统地降低并明显地升高,并且对于x = 0.0344,其达到658cm-1的值。 x = 0.0、0.0206和0.0344的矫顽力Hc(剩磁Mr)被确定为分别为995Oe(0.44emu / mg),1404Oe(0.00019emu / mg)和2023Oe(0.00016emu / mg)。 Ti掺杂样品的较大矫顽力可归因于其增强的形状和磁晶各向异性。从室温M?ssbauer数据观察到的异构体位移(δ)清楚地表明存在铁(Fe3 +)和Ti4 +离子,说明在α-Fe2?xTixO3赤铁矿中x的强铁磁有序直至x = 0.0206,而α-Fe2的铁磁有序较弱x = 0.0344的ΔxTixO3。

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