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Title: Formation of invariant plain-strain and tent-shaped surface reliefs by the diffusional ledge mechanism

Journal Article · · Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States)
OSTI ID:6935820
 [1];  [2]
  1. Univ. of Birmingham (United Kingdom). School of Metallurgy and Materials
  2. Geo-Centers, Inc., Ft. Washington, MD (United States)

Electron channeling contrast and electron backscattering patterns (EBSPs), generated in scanning electron microscopes (SEMs), were used to study the question of whether tent-shaped surface reliefs associated with ferrite plates in Fe-0.07 pct and Fe-0.50 pct C low-alloy steels are single crystals or back-to-back pairs of plates. Although more than 50 ferrite plates were examined in detail, any misorientation contained within them must have been <1 deg. Additionally, no sightings of the low-angle grain boundaries approximately bisecting ferrite plates expected on the back-to-back plates mechanism were ever made. The efforts of previous investigators to explain tent-shaped (and invariant plane-strain) reliefs on the basis of diffusional ledgewise growth were further extended.

OSTI ID:
6935820
Journal Information:
Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States), Vol. 25:9; ISSN 0360-2133
Country of Publication:
United States
Language:
English