Thermally induced changes in the magnetic properties of iron oxide nanoparticles under reducing and oxidizing conditions

被引:8
作者
Ponomar, V. P. [1 ]
Antonenko, T. S. [1 ]
Vyshnevskyi, O. A. [1 ]
Brik, A. B. [1 ]
机构
[1] NAS Ukraine, MP Semenenko Inst Geochem Mineral & Ore Format, Kiev, Ukraine
关键词
Iron oxide nanoparticles; Phase transformation; Magnetic properties; FeOOH; -; Fe2O3; Fe3O4; CHEMICAL REMANENT MAGNETIZATION; MAGHEMITE GAMMA-FE2O3; HEMATITE; REDUCTION; TRANSFORMATION; FE3O4; LEPIDOCROCITE; PARTICLES; REMOVAL; ORES;
D O I
10.1016/j.apt.2020.04.021
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Application of iron oxide nanoparticles in the fields of water purification, biomedicine or chemistry often requires controlled magnetic properties that can be modified by changing temperature and redox conditions. Therefore, this work investigates the changes in the magnetic properties of iron oxide nanoparticles in the FeOOH - Fe2O3 - Fe3O4 system (i.e. hematite, goethite, lepidocrocite, maghemite and magnetite) at heating under reducing and oxidizing conditions. The results show that heat treatment of hematite and goethite in the presence of a reducing agent (5% starch) leads to their conversion into high magnetic magnetite. The starting temperature of transformation is approximately 350 degrees C for both samples. The magnetization increases to 86 Am-2/kg for hematite reduced at 700 degrees C and to 88 Am-2/kg for goethite reduced at 900 degrees C. An intense reaction occurs within the first 10 min and then the conversion process decelerates. Thermal treatment of lepidocrocite under both oxidizing and reducing conditions leads to an increase in magnetization due to the formation of maghemite and magnetite, respectively. Regardless of the redox conditions, the formation of magnetic phase begins at a temperature of 250 degrees C and is associated with the formation of maghemite from lepidocrocite. Under oxidizing conditions, the magnetization begins to decrease at 350 degrees C, which is associated with the conversion of maghemite to hematite. On the contrary, under reducing conditions, the magnetization of lepidocrocite increases up to 900 degrees C, which is associated with the formation of magnetite. Maximum values of magnetization are 36 Am-2/kg for maghemite obtained at 350 degrees C, and 88 Am-2/kg for magnetite obtained at 900 degrees C from lepidocrocite. With the help of conventional heating, the magnetic properties of IONs can be altered by phase transformations in the FeOOH - Fe2O3 - Fe3O4 system. Temperature and redox conditions are the two most important factors controlling the transformation pathways and the magnetic properties of the resulting IONs. (C) 2020 The Society of Powder Technology Japan. Published by Elsevier B.V. and The Society of Powder Technology Japan. All rights reserved.
引用
收藏
页码:2587 / 2596
页数:10
相关论文
共 32 条
  • [1] Optimization of heavy metal removal from aqueous solutions by maghemite (γ-Fe2O3) nanoparticles using response surface methodology
    Ahmadi, Ali
    Heidarzadeh, Shahriar
    Mokhtari, Ahmad Reza
    Darezereshki, Esmaeil
    Harouni, Houshang Asadi
    [J]. JOURNAL OF GEOCHEMICAL EXPLORATION, 2014, 147 : 151 - 158
  • [2] Water purification using magnetic assistance: A review
    Ambashta, Ritu D.
    Sillanpaa, Mika
    [J]. JOURNAL OF HAZARDOUS MATERIALS, 2010, 180 (1-3) : 38 - 49
  • [3] A comparative study of nanosized iron oxide particles; magnetite (Fe3O4), maghemite (γ-Fe2O3) and hematite (α-Fe2O3), using ferromagnetic resonance
    Can, Musa Mutlu
    Coskun, Mustafa
    Firat, Tezer
    [J]. JOURNAL OF ALLOYS AND COMPOUNDS, 2012, 542 : 241 - 247
  • [4] Preparation of magnetic Fe3O4 particles modified sawdust as the adsorbent to remove strontium ions
    Cheng, Zihong
    Gao, Zhanxian
    Ma, Wei
    Sun, Qi
    Wang, Baodong
    Wang, Xiaoguang
    [J]. CHEMICAL ENGINEERING JOURNAL, 2012, 209 : 451 - 457
  • [5] Cornell RM., 2003, IRON OXIDES STRUCTUR, DOI DOI 10.1002/3527602097
  • [6] Low-temperature behaviour of haematite: susceptibility and magnetization increase on cycling through the Morin transition
    de Boer, CB
    Mullender, TAT
    Dekkers, MJ
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2001, 146 (01) : 201 - 216
  • [7] Dunlop D., 1997, Cambridge Studies in Magnetism, V3, DOI [10.1017/CBO9780511612794, DOI 10.1017/CBO9780511612794]
  • [8] Chemical reduction of hematite with starch
    M. S. Ellid
    Y. S. Murayed
    M. S. Zoto
    S. Musić
    S. Popović
    [J]. Journal of Radioanalytical and Nuclear Chemistry, 2003, 258 (2) : 299 - 305
  • [9] Removal of nitrate from drinking water using nano SiO2-FeOOH-Fe core-shell
    Ensie, Bekhradinassab
    Samad, Sabbaghi
    [J]. DESALINATION, 2014, 347 : 1 - 9
  • [10] Hematite to magnetite reduction monitored by Mossbauer spectroscopy and X-ray diffraction
    Gaviria, J. P.
    Bohe, A.
    Pasquevich, A.
    Pasquevich, D. M.
    [J]. PHYSICA B-CONDENSED MATTER, 2007, 389 (01) : 198 - 201