在雪裂实验中对裂传播模式的数值研究
Grégoire Bobillier1,2, Bastian Bergfeld1, Jürg Dual3
1WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland.
概括
雪崩裂的传播取决于斜率角度,速度在两个不同的模式下变化. 研究结果揭示了雪的特性如何影响裂动力学和断裂力学.
科学领域:
- 雪的物理 雪的物理
- 雪崩的动态 雪崩的动态
- 计算力学是计算力学.
背景情况:
- 雪崩释放涉及弱雪层中裂的传播.
- 了解雪的机械特性对裂动态的影响是有限的.
- 缺乏微机械分析的非侵入性方法.
研究的目的:
- 分析雪地覆盖特性对薄弱雪层裂传播动态的影响.
- 使用DEM模型调查裂传播的微机械方面.
- 确定影响稳定状态裂纹速度的因素.
主要方法:
- 使用离散元素方法 (DEM) 模型来模拟裂传播.
- 专注于在不同条件下分析稳定状态裂纹速度.
- 进行了微机械应力分析.
主要成果:
- 根据斜率角度确定了两个不同的断裂过程模式.
- 在平坦的地形上,裂纹速度取决于弹性模块和弱层强度 (高达剪切波速度的0.6倍).
- 在的斜坡上,观察到一个超级剪切模式 (约. 1.6倍剪波速度),由剪应力驱动.
结论:
- 雪地覆盖的特性显著影响动态裂传播的微力学.
- 斜坡角度是决定断裂模式和裂纹速度的关键因素.
- 一个半经验模型可以在某些条件下预测裂纹速度.
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