In order to explore the origin of the metal–insulator (M–I) transition, the precise crystal structures of the hole-doped Mott insulator system, Y 1- x Ca x TiO 3 ( x =0.37, 0.39 and 0.41), are studied for the temperature range between 20 K and 300 K by synchrotron radiation (SR) X-ray powder diffraction. For both Y 0.63 Ca 0.37 TiO 3 and Y 0.61 Ca 0.39 TiO 3 compositions, the orthorhombic ( P b n m ) – monoclinic ( P 2 1 / n ) structural phase transition occurs at approximately 230 K, which is much higher than their individual M–I transition temperatures, i.e., 60 K and 130 K, respectively. For these compositions, significant phase separation (low-temperature orthorhombic + monoclinic) is also found in the vicinity of the M–I transition temperature. On the other hand, Y 0.59 Ca 0.41 TiO 3 , which does not exhibit M–I transition and preserves a metallic behavior down to 1.5 K, is in a two phase state from 20 K to 300 K. It is concluded that the existence of the phase separation causes the M–I transition in Y 1- x Ca x TiO 3 , and the low-temperature orthorhombic phase contributes to the metallic property of this system.
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