Study of magnetization of ferrite with Rare Earth and Ca substitutions

N. Wendri, W. Suharta
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Abstract

This research synthesized nano-ferrite with Rare Earth substitution using the co-precipitation method. The main goal was to produce nanometer-sized RE/Ca-(Fe3O4) ferrite utilizing sand as the primary raw material. This research also sought to generate public interest in natural resources to maximize their benefits. Sand is abundantly available in Indonesia and is commonly used in the production of concrete, bricks, and roads. To obtain nanometer-scale particles, the co-precipitation method was employed in this study. Initially, iron sand was dissolved in HCl, stirred until homogeneous, filtered and NH4OH was added. The mixture was then precipitated, filtered and washed through a repetitive process until the nano-ferrite particles were obtained. To enhance the magnetic properties, rare earth elements (RE) were introduced during the ferrite formation. The results of FTIR characterization revealed absorbance at 1000, 1400, 1600 and 3400 cm-1, indicating vibrations caused by stretching vibrations of the metal-oxygen tetrahedral band, stretching and HOH vibrations of anti-symmetrical NO stretching vibrations arising from the nitrate group still present in the sample. XRD characterization demonstrated a spectrum predominantly composed of RE/Ca-(Fe3O4) with a purity exceeding 90%, along with the detection of SiO2 impurities. Substitution of Gd, GdNd, and Nd results in an increase in lattice constant values for the a, and b-axis, however, decrease for c-axis sequentially. Also, the substitution of Gd, GdNd, and Nd results in an increase in the coercivity and remanence magnetization values sequentially. The average particle size obtained was 150 nm.
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稀土和钙取代铁氧体磁化的研究
本研究采用共沉淀法合成了稀土取代纳米铁氧体。主要目标是利用砂作为主要原料生产纳米级RE/Ca-(Fe3O4)铁氧体。这项研究还试图引起公众对自然资源的兴趣,使其利益最大化。沙子在印度尼西亚储量丰富,通常用于生产混凝土、砖块和道路。为了获得纳米级颗粒,本研究采用共沉淀法。首先,将铁砂溶解在HCl中,搅拌至均匀,过滤后加入NH4OH。然后将混合物沉淀、过滤并通过重复过程洗涤,直到获得纳米铁氧体颗粒。为了提高磁性能,在铁氧体形成过程中引入稀土元素。FTIR表征结果显示,在1000、1400、1600和3400 cm-1处有吸光度,表明金属氧四面体带的拉伸振动引起了振动,样品中仍然存在的硝酸盐基引起了反对称NO拉伸振动的拉伸和HOH振动。XRD表征表明,其光谱主要由RE/Ca-(Fe3O4)组成,纯度超过90%,同时检测到SiO2杂质。Gd、GdNd和Nd的替换导致a轴和b轴的晶格常数值增加,而c轴的晶格常数值依次减少。此外,Gd、GdNd和Nd的取代导致矫顽力和剩磁值依次增加。得到的平均粒径为150 nm。
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