应变率对岩石强度和变形性质的影响
The Effect of Strain Rate on Strength aud Deformability of Rock
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摘要: 本文根据晶屑凝灰岩、石英砂岩、粉砂岩等在不同应变率下的压缩或拉伸试验结果,并结合国外的大量试验资料,得出岩石破坏强度发生显著变化的应变率范围ε_d;应变率小于ε_d时,随着应变率的变化,岩石强度无明显变化;应变率达到或超过ε_d时,岩石强度就有显著增长,对此用破裂传播速度作了理论分析和解释。另外根据岩石破坏前变形随应变率增大或减小的现象,提出了不同岩石具有不同的临界应变率。用该临界应变率可以确定岩石破坏后区的变形是随荷载的减小而呈增大或减小的变化趋势,并对此观象用破坏能的概念进行了探讨。本文还研究了软岩、硬岩对应变率的敏感度;并指出增大试件围压会使试件的应变率敏感度减弱,也就是说使试件趋于“硬化”。以上结论及理论分析不仅在理论上具有重要的意义,在岩石工程中也有实用意义。Abstract: Compressive or tensile tests were conducted on crystal tuff, silicarenite, and silts-tone samples under different strain rates,and also a great amount of literature consulted,it was found that the strength of rock rmains constant when strain rate varies from 10-4 (sec.-1) to 10-1 (sec.-1), and above 10-1 or 100 (sec.-1), the strength will increase obviously, and the cause of which can be explained by analyzing the fracture propagation in rock specimen.According to the phenomena that the pre-failure deformation increases or decreases with strain rate, a critical strain rate conception was postulated for studying the post-failure properties of rock.Also, the strain rate sensitivity for both hard rock and soft rock was examined.It was found that the strain rate sensitivity will decrease with the increase of confi-nning pressure on rock.