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在高度多孔的材料中混合模式抗裂的断裂性
Valentin Adam1,2, Bastian Bergfeld2, Philipp Weißgraeber3
1Institute of Structural Mechanics and Design, Department of Civil and Environmental Engineering, Technical University of Darmstadt, Franziska-Braun-Str. 3, 64285, Darmstadt, Germany.
Nature communications
|September 2, 2024
概括
在多孔材料中,如雪,破裂性抵御压缩下的抗裂变生长. 这项研究量化了跨剪切和崩模式的阻力,揭示了抗裂传播的功率定律关系.
科学领域:
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
- 断裂力学 断裂力学 断裂力学
背景情况:
- 多孔材料可以通过压力负载下的抗裂纹失效,导致结构失效.
- 抗裂增长阻力由裂性控制,类似于其他裂类型.
- 在合并剪切和压缩下,多孔材料的抗裂纹混合模式断裂性仍然未得到量化.
研究的目的:
- 为了实验性地确定自然积雪层薄弱层中的抗裂变生长的混合模式断裂性.
- 为了研究不同剪切和压缩比下的抗裂纹传播模式之间的关系.
- 为验证多孔材料故障的计算模型提供数据.
主要方法:
- 实地实验是在自然积雪层中的弱层上进行的.
- 进行了断裂机械测试,以模拟抗裂纹启动和传播.
- 使用机械模型来解释实验数据并计算断裂性值.
主要成果:
- 断裂性被量化为抗裂变增长在各种模式相互作用的频谱,从纯切割到纯崩.
- 与崩主导的故障相比,在剪切主导的故障中观察到明显更高的断裂性值.
- 在不同的抗裂纹传播模式之间确定了一种电力定律关系.
结论:
- 该研究提供了第一次测量混合模式断裂性,用于天然多孔材料 (雪包) 中的抗裂纹.
- 结果表明,剪切和崩模式之间的断裂阻力有明显的差异,受力规律相互作用的支配.
- 这些发现为抗裂纹的断裂机制提供了关键的见解,并为数值模拟建立了基准.
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