易碎材料在压力失效时的通用行为
1Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire 03755, USA. carl.renshaw@darmouth.edu
Nature
|August 31, 2001
概括
岩石和冰中的脆性故障受到裂启动和传播的限制. 一个新的定量模型用可测量的机械参数解释了脆性-柔性过渡和压力强度.
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
- 固体力学 固体力学是什么
背景情况:
- 脆性故障在快速加载和低限制下限制了岩石和冰的压力强度.
- 柔软性故障发生在较高的限制或较慢的负载时,穿过脆性-柔软性过渡.
- 现有的脆弱故障定位模型包括机翼裂连接或微柱曲.
研究的目的:
- 分析在晶体材料中的脆性故障定位的拟议机制.
- 开发一种关于脆性压力强度和脆性-柔性过渡的定量模型.
- 为普遍的脆性故障过程提供证据.
主要方法:
- 在二次裂之间的微柱中分析曲诱导的故障机制.
- 基于可测量的机械参数的封闭形式定量模型的开发.
- 将模型预测与来自各种晶体材料的实验数据进行比较.
主要成果:
- 拟议的机制解释了在低到中等限制条件下的脆性故障局部化.
- 开发的模型准确地预测了脆脆的压力强度.
- 模型预测与不同材料的脆性-柔性过渡的实验数据保持一致.
结论:
- 该研究提出了基于微柱曲的脆性故障的定量模型.
- 该模型与实验数据一致,支持通用脆性故障过程.
- 这些发现强调了该模型对晶体材料的广泛适用性.
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