AI Article Synopsis

  • The process zone at the tip of a crack changes shape from concave to convex as the crack velocity increases, eventually forming a dropletlike configuration with a metastable wake.
  • The transformation of this zone starts when the crack velocity exceeds a specific speed, known as Gordon's speed (V_G), which marks the transition between stable and unstable phases.
  • As the crack's velocity rises, the size of the process zone decreases significantly, while the length of the direct contact between the zone and the crack surface varies, peaking at V_G before declining past a critical speed (V_cr).

Article Abstract

The morphological transformation of the process zone at the tip of a propagating crack occurs with the increase of the crack velocity. The zone configuration changes its shape from concave to convex, dropletlike form. The latter exhibits a metastable wake. We prove that the transformation takes place as soon as the crack velocity exceeds Gordon's speed V_{G}. The latter is the velocity of motion of the interface between the stable and overheated metastable phases. We further analyze the dependence of geometrical parameters of the zone and wake on the crack tip velocity. We show that at a constant velocity, the size of the process zone grows with the approach to the binodal. However, it decreases by over three orders of magnitude as the crack's velocity increases. In contrast, the interval length where the zone or the wake comes in direct contact with the crack surface increases at 0≤V

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Source
http://dx.doi.org/10.1103/PhysRevE.101.033004DOI Listing

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