DISLOCATION STRUCTURE IN "AS-GROWN" HIGH-PURITY IRON SINGLE CRYSTALS

1967 ◽  
Vol 45 (2) ◽  
pp. 1041-1045 ◽  
Author(s):  
S. Kadečková ◽  
B. Šesták

The dislocation structure in iron single crystals prepared by two different strain–anneal techniques from the starting material of two different purities is studied by the method of etch pits. Average dislocation densities of 2.6 × 105 to 7 × 105 cm−2 and the absence of subboundaries are observed in single crystals grown statically or dynamically from zone-refined Johnson and Matthey spectrographic iron. The presence of broad subboundaries and average dislocation densities of 8.6 × 105 to 3.3 × 106 cm−2 is characteristic for single crystals grown from the non–zone-refined J. and M. iron. Annealing of "as-grown" crystals does not greatly influence the dislocation structure. It is assumed that the impurities are mainly responsible for the observed dislocation densities.

1986 ◽  
Vol 34 (2) ◽  
pp. 823-836 ◽  
Author(s):  
Yong-Ki Park ◽  
James T. Waber ◽  
Michael Meshii ◽  
C. L. Snead ◽  
C. G. Park

1966 ◽  
Vol 16 (1) ◽  
pp. 89-94 ◽  
Author(s):  
B. Šesták ◽  
S. Kadečková

1988 ◽  
Vol 105 (1) ◽  
pp. K37-K40 ◽  
Author(s):  
P. P. Pal-Val ◽  
V. D. Natsik ◽  
S. Kadečková

1990 ◽  
Vol 31 (2) ◽  
pp. 118-128 ◽  
Author(s):  
J. Kumagai ◽  
S. Takaki ◽  
S. Suzuki ◽  
H. Kimura

1984 ◽  
Vol 19 (6) ◽  
pp. 781-791 ◽  
Author(s):  
V. Novák ◽  
S. Kadečková ◽  
B. Šesták ◽  
N. Zárubová

An account is given of the deformation and fracture characteristics of single crystals of high-purity iron of various orientations when tested in tension at temperatures from 100 to ─253°C. At temperatures down to ─124°C, the crystals were fully ductile, giving chisel-edge fractures and 100% reduction in area. At ─196°C, depending on the orientation of the stress axis, the behaviour covered the whole range from fully ductile with 100% reduction in area to completely brittle with cleavage fractures and no apparent deformation. Between these limits, mixtures of slip, twinning and cleavage were obtained. At ─253°C, the crystals gave cleavage fractures, and, over most of the orientation range studied, this occurred without prior deformation. It is shown that the resolved shear stresses required to produce slip or twinning at ─196°C vary with the orientation; in particular, the values are higher for orientations within 20 to 25° of the [001] than elsewhere in the unit triangle, and these values are not reached in this region before failure occurs by cleavage. A mechanism is put forward to explain this in terms of ‘locking’ of dislocations. The cleavage strength resolved normal to the cleavage plane is not constant with change in temperature, as is commonly supposed, but is substantially higher at ─253°C than at ─196°C.


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