Dislocation dynamics modelling of the creep behaviour of particle-strengthened materials

被引:17
|
作者
Liu, F. X. [1 ]
Cocks, A. C. F. [2 ]
Tarleton, E. [1 ,2 ]
机构
[1] Univ Oxford, Dept Mat, Parks Rd, Oxford OX1 3PH, England
[2] Univ Oxford, Dept Engn Sci, Parks Rd, Oxford OX1 3PJ, England
基金
英国工程与自然科学研究理事会;
关键词
particle; self-climb; cross-slip; creep; CROSS-SLIP; SINGLE-CRYSTALS; ELASTIC FIELD; CLIMB; PLASTICITY; INCLUSION; STRESS; SCREW; LOOPS; DEFORMATION;
D O I
10.1098/rspa.2021.0083
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Plastic deformation in crystalline materials occurs through dislocation slip and strengthening is achieved with obstacles that hinder the motion of dislocations. At relatively low temperatures, dislocations bypass the particles by Orowan looping, particle shearing, cross-slip or a combination of these mechanisms. At elevated temperatures, atomic diffusivity becomes appreciable, so that dislocations can bypass the particles by climb processes. Climb plays a crucial role in the long-term durability or creep resistance of many structural materials, particularly under extreme conditions of load, temperature and radiation. Here we systematically examine dislocation-particle interaction mechanisms. The analysis is based on three-dimensional discrete dislocation dynamics simulations incorporating impenetrable particles, elastic interactions, dislocation self-climb, cross-slip and glide. The core diffusion dominated dislocation self-climb process is modelled based on a variational principle for the evolution of microstructures, and is coupled with dislocation glide and cross-slip by an adaptive time-stepping scheme to bridge the time scale separation. The stress field caused by particles is implemented based on the particle-matrix mismatch. This model is helpful for understanding the fundamental particle bypass mechanisms and clarifying the effects of dislocation glide, climb and cross-slip on creep deformation.
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页数:24
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