Berman Neri, Cohen Gil, Fineberg Jay
The Racah Institute of Physics, The Hebrew University of Jerusalem, Jerusalem 91904, Israel.
Phys Rev Lett. 2020 Sep 18;125(12):125503. doi: 10.1103/PhysRevLett.125.125503.
The cohesive zone is the elusive region in which material fracture takes place. Here, the putatively singular stresses at a crack's tip are regularized. We present experiments, performed on PMMA, in which we visualize the cohesive zone of frictional ruptures as they propagate. Identical to shear cracks, these ruptures range from slow velocities to nearly the limiting speeds of cracks. We reveal that the cohesive zone is a dynamic quantity; its spatial form undergoes a sharp transition between distinct phases at a critical velocity. The structure of these phases provides an important window into material properties under the extreme conditions that occur during fracture.
内聚区是材料发生断裂的难以捉摸的区域。在这里,裂纹尖端假定的奇异应力被正则化。我们展示了在聚甲基丙烯酸甲酯(PMMA)上进行的实验,在实验中我们观察了摩擦破裂的内聚区在扩展时的情况。与剪切裂纹相同,这些破裂的速度范围从低速到接近裂纹的极限速度。我们发现内聚区是一个动态量;其空间形态在临界速度下会在不同阶段之间发生急剧转变。这些阶段的结构为了解断裂过程中出现的极端条件下的材料特性提供了一个重要窗口。