In situ X-ray diffraction reveals that hydrothermal synthesis of SrFe12O19 always proceeds through a ferrihydrite (FeOOH) intermediate that influences the magnetic behavior of the final material.
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Unraveling structural and magnetic information during growth of nanocrystalline SrFe12O19
In situ X-ray diffraction reveals that hydrothermal synthesis of SrFe12O19 always proceeds through a ferrihydrite (FeOOH) intermediate that influences the magnetic behavior of the final material.