Magnetic particulates in the environment, collected from surfaces and directly from the atmosphere, are reported. A significant percentage of magnetic material in many air-borne samples consists of spherical magnetite from coal-burning utilities and from iron/steel manufacturing with particle diameters 2–10 μm which correspond to average coercive fields of ∼100 Oe and remanence to saturation ratios of ∼0.1. The amount of air-borne magnetic material that settles to the ground varies inversely with distance from its source.
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P. J. Flanders (1994) studied this question.
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