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Strain localization in a continuum as an instability event

机译:应变局部化为不稳定性事件

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The paper presents a novel physical model, based on perturbation theory, to describe localization pattern formation in a solid material as a result of system instabilities. Such kind of approach has been inspired by the theory of population dynamics. In particular, the sinergetic phenomenon of strain localization into a stressed continuum, and its subsequent evolution to cohesive cracking, is obtained through the competition of an external source of energy (e.g., strain energy) and of the internal behavior of the material. The hypothesis of mobile energy entities within material bulk is put forward. These entities, which under low strain conditions are evenly distributed throughout the body, can be considered as strain quanta. The quantization of mechanical quantities is not new in continuum and fracture mechanics, [see, e.g., Novozhilov (1969, Prik Mat Mek 33:212–222)]. With increasing strain, a certain critical point is reached when the homogeneous situation becomes unstable and the strain quanta begin to aggregate into bands, leading to periodic strain localization patterns. The model, which is only theoretical at this stage, can be applied to the particular case of dry snow avalanches. In these cases, snow avalanche triggering is due toinstability (onset of sliding onto a weak plane) and is controlled by external loading (e.g., weight of the slope, load by skiers) and by internal factors (e.g., temperature changes, snow phase transformations etc.).
机译:本文介绍了一种基于扰动理论的新型物理模型,用于描述由于系统不稳定而在固体材料中形成的定位图案。这种方法受到人口动态理论的启发。特别是,通过外部能量(例如,应变能)和材料的内部行为的竞争,获得了应变局部化为应力连续体的单脉冲现象,以及随后演变为粘结裂纹的现象。提出了物质内部的移动能实体的假说。这些在低应变条件下均匀分布在整个身体中的实体可以视为应变量子。在连续力学和断裂力学中,机械量的量化并不是新事物,[参见,例如,Novozhilov(1969,Prik Mat Mek 33:212–222)]。随着应变的增加,当均匀状态变得不稳定并且应变量子开始聚集到带中时,会达到某个临界点,从而导致周期性应变局部化。该模型在此阶段仅是理论上的,可以应用于干燥雪崩的特殊情况。在这些情况下,雪崩触发是由于不稳定性(开始滑动到薄弱的平面上)引起的,并且受外部负载(例如,斜坡的重量,滑雪者的负载)和内部因素(例如,温度变化,雪相转变)的控制等等。)。

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