Abstract

The optical absorption spectra from bismuth ferrite (BiFeO 3 ) have been studied at high pressures up to 60 GPa in diamond anvil cells. An electronic transition at which the energy of the optical absorption edge decreases sharply from ~1.5 eV to zero has been observed at room temperature in a pressure range of 45‐55 GPa. This indirectly indicates a insulator‐metal transition. The observed electronic transition correlates with the recently revealed structural and magnetic transitions induced by high pressures in this crystal. The behavior of the optical absorption edge with decreasing the pressure is completely reversible in correlation with the reversibility of the magnetic transition. The “smearing” of the structural transition in pressure is caused by thermal fluctuations between the high-spin state and low-spin state of the Fe 3+ ions near the transition.

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