Magnetite in soils: I. The synthesis of single-domain and superparamagnetic magnetite
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AbstractA series of experiments has been carried out to investigate the possible formation of magnetite, Fe3O4, under ambient soil-forming conditions. Rapid and easy synthesis of magnetite was achieved through controlled oxidation of Fe2+ solutions at room temperatures and near neutral pH values. The synthetic products were found to range in size between 0·01–0·07 µm (mean diameter) and hence span the theoretical superparamagnetic-single-domain grain-size boundary.
1994 ◽
Vol 52
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pp. 620-621
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1992 ◽
Vol 55
(1)
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pp. 23-27
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2015 ◽
Vol 645-646
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pp. 145-150
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2004 ◽
Vol 38
(5)
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pp. 1569-1575
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