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arxiv: 1006.0126 · v1 · pith:3TAB3XAOnew · submitted 2010-06-01 · ❄️ cond-mat.supr-con

Th substituted SmFeAsO: structural details and superconductivity with Tc above 50 K

classification ❄️ cond-mat.supr-con
keywords samplescriticalcrystalsdecreasingfieldgammamagneticsingle
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Superconducting poly- and single-crystalline samples of Sm1-xThxFeAsO with partial substitution of Sm3+ by Th4+ were synthesized and grown under high pressure and their structural, magnetic and transport properties are studied. The superconducting Tc reaches values higher than 50 K. Bulk superconducting samples (x = 0.08, 0.15, 0.3) do not show any signs of a phase transition from tetragonal to orthorhombic crystal structure at low temperatures. With Th substitution the unit cell parameters a and c shrink and the fractional atomic coordinate of the As site zAs remains almost unchanged, while that of Sm/Th zSm/Th increases. Upon warming from 5 K to 295 K the expansion of the FeAs layer thickness is dominant, while the changes in the other structural building blocks are smaller by a factor of 1/5, and they compensate each other, since the As-Sm/Th distance appears to contract by about the same amount as the O-Sm/Th expands. The poly- and single-crystalline samples are characterized by a full diamagnetic response in low magnetic field, by a high intergrain critical-current density for polycrystalline samples, and by a critical current density of the order of 8 x 105 A/cm2 for single crystals at 2 K in fields up to 7 T. The magnetic penetration depth anisotropy {\gamma}{\lambda} increases with decreasing temperature, a similar behavior to that of SmFeAsO1-xFy single crystals. The upper critical field estimated from resistance measurements is anisotropic with slopes of 5.4 T/K (H//ab plane) and 2.7 T/K (H//c axis), at temperatures sufficiently far below Tc. The upper critical field anisotropy {\gamma}H is in the range of 2, consistent with the tendency of a decreasing {\gamma}H with decreasing temperature, already reported for SmFeAsO1-xFy single crystals.

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