Ductile fracture initiation in pure α-Fe: Part I. Macroscopic observations of the deformation history and failure of crystals |
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Authors: | R N Gardner H G F Wilsdorf |
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Affiliation: | (1) Central Research Laboratories, 3M Company, 3M Center, 55101 St. Paul, MN;(2) School of Engineering and Applied Science, University of Virginia, 22901 Charlottesville, VA |
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Abstract: | Single crystalα-Fe whiskers, grown by the reduction of ferrous chloride by hydrogen have been strained to fracture in an Instron tensile
testing machine and in a bench straining device at various elongation rates at room temperature. Whiskers were found to exhibit
macroscopic slip behavior strongly dependent upon elongation rate while the geometric reduction in area and the fracture mode
remained in all cases identical. Ductile rupture of iron whiskers produces a characteristically shaped chisel-edge fracture
whose geometry is sensitive to crystal orientation, due to the geometry of active slip systems, but which isnot a function of strain rate. The micromechanisms of ductile rupture of these single crystals are strongly affected by dislocation
dynamics. The development of dislocations necessary to accomodate an extensive reduction in area appears to be independent
of the nature of surface slip observed. Dislocation structures form small volume elements which are separated from one another
by dislocation cell walls. The accommodation of large strains as well as the reduction in area is determined by the movement
of dislocations on the order of a distance equal to that of the dislocation cell size. The boundaries of the cell and/or the
cell volume could then be expected to be specifically related to the site where the initiation of fracture occurs. |
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