层叠材料中断裂间距的解释
1Department of Geological and Environmental Sciences, Stanford University, California 94305-2115, USA. bai@pangea.stanford.edu
Nature
|February 29, 2000
概括
在分层材料中的断裂间距最初会随着应变而减少,但随后会稳定,这种现象称为断裂和. 这项研究揭示了导致这种和的潜在压力过渡,与之前的理论形成鲜明对比.
科学领域:
- 地质力学 地质力学
- 材料科学 材料科学 材料科学
- 岩石物理 岩石物理
背景情况:
- 有层的材料呈现出与层厚度成比例的断裂间距.
- 现有的断裂理论不能完全解释断裂和.
- 骨折和发生在新的骨折停止形成和现有骨折扩大时.
研究的目的:
- 研究分层材料中断裂之间的全应力分布.
- 开发骨折和的物理模型.
- 解释骨折之间从拉力压力过渡到压力压力.
主要方法:
- 数字模拟的数字模拟.
- 实验室实验 实验室实验 实验室实验
- 对应力分布的分析.
主要成果:
- 观察到从拉力到压力正常应力之间的断裂与增加施加应力之间的过渡.
- 证明裂纹间距尺度与和后的层厚度.
- 开发了一个物理模型来解释断裂和.
结论:
- 正常压力的过渡是骨折和的原因.
- 由此衍生的物理模型提供了对断裂和的直观理解.
- 这些发现在地质科学和工程领域具有广泛的应用.
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