Abstract
The study of fine-particle magnetism is of importance because of the natural abundance of various fine-particle materials, and because the special properties of finely divided materials lead to their utilization in a wide range of manufactured goods. Naturally occurring fine particles include the chains of magnetite particles found in magnetotactic bacteria, the several grams of iron stored in the human body as the ferrihydrite cores of storage proteins, and the magnetic phases and weathering products found in rocks, soils, and coals. Manufactured magnetic fine particles include the magnetite particles used in fluid seals and bearings, and the particles of maghemite, barium ferrite, and others used in computer hard and floppy disks, credit cards, and audio and video recording tapes.
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Pankhurst, Q.A., Pollard, R.J. (1993). Applied Field Mössbauer Spectroscopy of Magnetic Powders. In: Long, G.J., Grandjean, F. (eds) Mössbauer Spectroscopy Applied to Magnetism and Materials Science. Modern Inorganic Chemistry, vol 1. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-2409-4_3
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