Reversed gyroremanent magnetization in γ-Fe2O3 participate systems

Tiberiu Salaoru, David K. Potter, Laurenţiu Stoleriu, Constantin Pǎpuşoi, Alexandru Stancu

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    3 Citations (Scopus)

    Abstract

    Gyroremanent magnetization (GRM) has previously been studied in connection with the well-known technique of ac demagnetization, which is used extensively in rock magnetism, palaeomagnetism and magnetic materials research. The "normal" GRM effect was explained by Stephenson in 1980, but recently a "reversed" GRM was obtained in a CrO2 particle system by Madsen. We have studied samples of ?-Fe2O3 particles (commercial magnetic recording tapes) and have identified samples with both "normal" and "reversed" GRM. The amplitude of the ac field was found to essentially influence the character of the GRM. In this paper, we also present micromagnetic simulations of the GRM in systems of single-domain particles and the results are discussed. Both "normal" and "reversed" GRM have been obtained in the simulations.

    Original languageEnglish
    Pages (from-to)2407-2409
    Number of pages3
    JournalIEEE Transactions on Magnetics
    Volume40
    Issue number4 II
    DOIs
    Publication statusPublished - Jul 2004

    Keywords

    • Gyroremanent magnetization (GRM)
    • Magnetization processes
    • Micromagnetic model
    • Particulate media
    • Rock magnetism

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  • Cite this

    Salaoru, T., Potter, D. K., Stoleriu, L., Pǎpuşoi, C., & Stancu, A. (2004). Reversed gyroremanent magnetization in γ-Fe2O3 participate systems. IEEE Transactions on Magnetics, 40(4 II), 2407-2409. https://doi.org/10.1109/TMAG.2004.830458