Abstract
The thermal diffusivities of oxide scales on iron, certain binary iron alloys, and selected commercial steels have been determined in situ at temperatures from 473 to 1273 K with a laser flash-pulse technique. The results confirmed that the thermal diffusivities were a function of the type of oxide and of its growth morphology. The greater the proportion of magnetite (Fe304) and free iron in a scale, the higher is the thermal diffusivity obtained (up to ∼ 9 x 10−7 m2 s−1). A scale/metal interfacial gap constitutes a thermal barrier possessing a correspondingly lower apparent thermal diffusivity (<1 X 10−7 m2 S−1). Consideration is given to the practical problem that the cooling rate for a blistered, scaled surface may be a factor of 5-50 times slower than that for a descaled steel surface.
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