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The magnetic properties of permanent strontium ferrite doped with rare-earth by chemical co-precipitation method

机译:化学共沉淀法掺杂稀土永锶铁素体的磁性

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摘要

The Sr1-xSmxFe12-xCuxO19 (0 = x = 0.2) materials were prepared by chemical co-precipitation technique. The products were characterized by X-ray diffraction (XRD), fourier transform infrared spectroscopy (FTIR), scanning electric microscopy (SEM) and vibrating sample magnetometer (VSM). The results of XRD showed that the pure M-type hexaferrites are obtained. The Sm3+ and Cu2+ ions were completely doped into strontium ferrite phase. With the increasing of Sm-Cu content, the grain size gradually increases. The FTIR spectra of annealed samples of Sr1-xSmxFe12-xCuxO19 showed that strontium hexaferrite particles have been successfully synthesized and M-type SrFe12O19 intrinsic crystal structure has not been destroyed. A filed emission scanning electric microscopy was employed to explore the micrographs of the magnets. The hexaferrite magnets have formed hexagonal-shaped crystals. The magnetic properties were tested by VSM. In the single M-type phase region, the variation of magnetic properties with Sm-Cu substitution amount is well explained based on the occupancy effect of Sm3+, Cu2+ in magnetoplumbite structure. The results indicate that the Br increases and then decrease when rare-earth content (x) continutes to increase. With the dosages of Sm-Cu from 0 to 0.20, the Hc at x = 0.15 reach the maximum value of 6862.62 Oe.
机译:通过化学共沉淀技术制备SR1-XSMXFE12-XCUXO19(0& = x& = 0.2)。该产品的特征在于X射线衍射(XRD),傅里叶变换红外光谱(FTIR),扫描电显微镜(SEM)和振动样品磁力计(VSM)。 XRD的结果表明,获得纯M型六峰流动素。将SM3 +和Cu 2 +离子完全掺杂到锶铁氧体相中。随着SM-Cu含量的增加,晶粒尺寸逐渐增加。 SR1-XSMXFE12-XCUXO19的退火样品的FTIR光谱表明,已成功合成六氢锶颗粒,并且M型SRFE12O19内在晶体结构未被破坏。采用归档发射扫描电显微镜探索磁铁的显微照片。六足磁铁具有形成六边形晶体。通过VSM测试磁性。在单一M型相位区域中,基于SM3 +,Cu2 +在磁压石结构中的占用效应很好地解释了具有SM-Cu取代量的磁性的变化。结果表明,当稀土含量(X)持续增加时,BR增加,然后减少。用0至0.20的SM-Cu的剂量,HC X = 0.15达到最大值6862.62 OE。

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