2013
DOI: 10.1134/s0031918x13100037
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Nature of anisotropy of impact toughness of structural steels with ferrite-pearlite structure

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Cited by 8 publications
(11 citation statements)
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“…It should be noted that such a dynamic adaptation of the material under the dynamic impact is a consequence of a self-organization of the polycrystalline material. At the same time, there is a self-organization of the structural-mechanical levels of deformation of local sections of the material into the energetically most favorable configuration under given loading conditions [20]. Increasingly large conglomerates of grains become involved in the deformation process, and deformational fragmentation of the material occurs at the meso-level [19,20].…”
Section: Shear Lipsmentioning
confidence: 99%
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“…It should be noted that such a dynamic adaptation of the material under the dynamic impact is a consequence of a self-organization of the polycrystalline material. At the same time, there is a self-organization of the structural-mechanical levels of deformation of local sections of the material into the energetically most favorable configuration under given loading conditions [20]. Increasingly large conglomerates of grains become involved in the deformation process, and deformational fragmentation of the material occurs at the meso-level [19,20].…”
Section: Shear Lipsmentioning
confidence: 99%
“…At the same time, there is a self-organization of the structural-mechanical levels of deformation of local sections of the material into the energetically most favorable configuration under given loading conditions [20]. Increasingly large conglomerates of grains become involved in the deformation process, and deformational fragmentation of the material occurs at the meso-level [19,20]. Failure of the material is the final stage of fragmentation, when the process transfers to the macro-level, followed by a global loss of shear stability.…”
Section: Shear Lipsmentioning
confidence: 99%
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“…T = −20 °C: The fracture mechanism is similar to that at T = 20 °C. The size of ductile fracture pits is slightly smaller (Figure 9b) [44,45]. T = −60 °C: The major fracture mechanism at this temperature was cleavage.…”
Section: Fracture Micromechanismsmentioning
confidence: 99%