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Creep behaviour of ice single crystals loaded in torsion explained by dislocation cross-slip

机译:错位错滑解释了扭转载荷下的冰单晶的蠕变行为

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摘要

Torsion creep experiments are carried out in order to understand the physics of ice plasticity. A dislocation spreading mechanism based on double cross-slip of basal dislocations is proposed to explain the strong plastic anisotropy and the power law relationship between stress and strain rates. The scenario is tested using three-dimensional dislocation dynamics simulations. Numerical investigations give a stress exponent n = 2.3 in agreement with experimental measurements. This dislocation spreading mechanism sheds a new light on the interpretation of former experimental observations.
机译:为了了解冰的可塑性,进行了扭转蠕变实验。为了解释强塑性各向异性以及应力与应变率之间的幂律关系,提出了一种基于基底位错的双重错位的位错扩展机制。该场景使用三维位错动力学模拟进行了测试。数值研究得出应力指数n = 2.3与实验测量结果一致。这种位错扩散机制为以前的实验观察的解释提供了新的思路。

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