Abstract

AbstractA pronounced influence of the molten zone stability on the dislocation substructure of as grown single crystals is found in Fe–3% Si alloys. In single crystals prepared by downward zoning the density of dislocations was ≅ 3 · 105 cm−2 and no local changes of mosaic structure are observed. On the other hand in single crystals prepared by upward zoning, where the molten zone is less stable than in the first case, considerable local changes in size and disorientation of mosaic blocks are found, crosswise and especially along the single crystals axis. The density of dislocations along the axis varied from ≅ 1 · 106 cm−2 to ≅ 3 · 106cm−2. The difference may be explained by dislocation generation due to the change of concentration gradients of impurities and due to the change of temperature gradients. Both are higher in crystals prepared by upward zoning than in those prepared by zone moving in the opposite direction.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.