微波处理下赤铁矿向磁铁矿的相变

IF 0.5 Q4 MINERALOGY Mineralogical Journal-Ukraine Pub Date : 2021-01-01 DOI:10.15407/mineraljournal.43.04.011
T. Antonenko, A. Brik, O.Yu. Tsymbal, N. O. Dudchenko, V. Ovsienko, Yu. I. Cherevko
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引用次数: 0

摘要

研究了天然赤铁矿和合成赤铁矿在含铁水介质中,在室温~ 260°С温度范围和6 MPa压力下的相变。初始样品的饱和磁化强度均小于1 A∙m2/kg,而相变后样品的饱和磁化强度显著增加(最高可达27 A·m2/kg)。x射线衍射表明,所有样品都转变为磁铁矿。测量了处理后样品的热磁曲线,并测定了居里温度。测定了天然赤铁矿样品的居里温度为560℃,合成赤铁矿样品的居里温度为559℃,接近纯磁铁矿的居里温度(580℃)。所获得的磁性颗粒的相对较高的饱和磁化强度使其具有不同的应用前景(放射性废物的吸附剂,磁性药物靶向载体等)。这项调查的结果也可用于开发从采矿和加工厂的含赤铁矿废物中生产铁矿石精矿的新技术。
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Phase Transformation of Hematite to Magnetite Under Microwave Treatment
Phase transformations of natural and synthetic hematite in aqueous Fe (II)-containing medium under the influence of microwave radiation at a temperature range from room temperature to 260°С and pressure of 6 MPa were investigated. The saturation magnetization of all initial samples was less than 1 A∙m2/kg, while the saturation magnetization of the samples after phase transformations increases significantly (i.e., up to 27 A·m2/kg). It was shown by X-ray diffraction that all samples were transformed into magnetite. Thermomagnetic curves were measured for the treated samples and Curie temperatures were determined. Curie temperatures of the samples of natural hematite were determined as 560 °C and for synthetic hematite as 559°C that are close to the Curie temperature of pure magnetite (580°C). The relatively high saturation magnetization of obtained magnetic particles makes them promising for different applications (adsorbents of radioactive waste, carriers for magnetic drug targeting, etc.). The results of this investigation could also be useful for developing new technologies for production of iron ore concentrates from the hematite-containing waste of mining and processing plants.
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来源期刊
CiteScore
0.70
自引率
0.00%
发文量
18
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