A Fe3O4/wood composite, a magnetic material, was prepared by in situ chemosynthesis at room temperature. X-ray diffraction (XRD), vibrating sample magnetometry (VSM) and Fourier transform infrared (FTIR) spectroscopy were applied to characterise the resulting products. The XRD results show that the average grain size of Fe3O4 was ∼14 nm. The VSM shows that the composites have saturation magnetisation Ms values from 4·7 to 25·3 emu g−1 with the increase in weight per cent gains of the wood for the composites, but the coercive forces Hc are invariable, which is different from the magnetic materials reported before. It may be due to the fact that the interaction between wood and Fe3O4 becomes stronger when less Fe3O4 particles are introduced in the composition, and this also changes the surface anisotropy Ks of the magnetism. Structural characterisation by FTIR proves the interaction between Fe3O4 particles and the wood matrix, and it also illustrates that this interaction influences the coercive force of the composite.
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