Microstructures of deformation and fracture of cementite in pearlitic carbon steels strained at various temperatures |
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Authors: | Akihisa Inoue Tsugio Ogura Tsuyoshi Masumoto |
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Affiliation: | (1) Research Institute for Iron, Steel and Other Metals, Tohoku University, Sendai, Japan |
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Abstract: | In order to make clear the effect of temperature on deformation and fracture of cementite in steels, observations by transmission
electron microscopy were made on cementite in carbon steels strained in tension at various temperatures ranging from -196
to 700°C. Hardly any plastic deformation of cementite was detected at-196 and-78°C. It was confirmed that above room temperature
cementite in steel can deform due to dislocation slip and that the deformation becomes easier as the temperature increases.
Slip in cementite at room temperature and at 300°C seems to be confined to only (100) or (001). Dislocations observed at room
temperature and at 300°C were mostly isolated and straight. Above 400°C (100), (010), (001), and some {110} planes are all
operative slip planes. Dislocation loops, dipoles, cusps, and networks were frequently found. These observations indicate
that double slipping and the interaction of dislocations can occur and that the deformability of cementite above 400°C is
very large. An appreciable degree of dynamic recovery was detected above 500°C. The fracture of cementite at -196 and-78°C
occurred in a cleavage manner along some crystallographic planes such as (110), (100) or (210). Above room temperature fracture
occurred along an activated slip plane and was preceded by some amount of slip on that plane. Above 400°C cementite fracture,
caused by joining of voids, formed along an activated slip plane was frequently observed. |
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