Abstract
An Fe–25Cr alloy was oxidized in Ar at 973 K with or without external stresses of 30, 35, and 40MPa. A 0.1-μm thick Cr2O3 scale was formed during pretreatment, after which it grew obeying a parabolic rate law without formation of flaws, i.e., cracks and exfoliation. After the pretreatment, tensile stresses of 30, 35, and 40 MPa were applied to monitor cracking behavior of the oxide scale. Cracking commenced at the alloy grain boundaries by the end of a second-stage creep. In a third stage, cracks formed in the alloy grains, arrayed almost perpendicular to the direction of the tensile stress, with regular intercrack spacings. The average intercrack spacings (L) at grain boundaries are smaller than the intercrack spacing of the grains, and the spacings are given by the power law relation: L∝(ε⋅)n, with strain rate exponents n of -0.22 for grains and −0.44 for grain boundaries. It appears that the local strain rate at grain boundaries is much larger than that of the grain as well as that the toughness of the oxide formed on the grain boundaries may be less than that of the grains. Indentation with a Vickers micro hardness tester indicated that the adhesion and fracture toughness of the oxide scale decreased both with growth of the oxide scale and creep deformation of the alloy substrate.
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Sohn, I.R., Narita, T. Cracking Behavior of Cr2O3 Scales on Fe–25Cr Alloys Under Creep Deformation at 973 K in Ar Atmosphere. Oxidation of Metals 59, 333–352 (2003). https://doi.org/10.1023/A:1023096128605
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DOI: https://doi.org/10.1023/A:1023096128605