Abstract
Measurements of temperature-dependent in-plane resistivity, , were used to determine the upper critical field and its anisotropy in high quality single crystals of stoichiometric iron arsenide superconductor KFeAs. The crystals were characterized by residual resistivity ratio, up to 3000 and resistive transition midpoint temperature, =3.8 K, significantly higher than in previous studies on the same material. We find increased for both directions of the magnetic field, which scale with the increased . This unusual linear scaling is not expected for orbital limiting mechanism of the upper critical field in clean materials.
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