The surface of a propagating crack is shown to be morphologically unstable because of the nonhydrostatic stresses near the surface (Asaro-Tiller-Grinfeld instability). We find that the energy of a wavy crack becomes smaller than the energy of a straight crack if the crack length is a few times larger than the Griffith length. The local dispersion relation is derived assuming that the instability develops via mass transport by surface diffusion. We also argue that the widely used condition of the vanishing of KII, the stress-intensity factor of the sliding mode, appears in a natural way in our description as an effective boundary condition at the tip of the crack. [S0031-9007(98)07834-X] The uniform motion of a straight crack is well understood [1]. Experiments on the fracture of bulk specimens, however, show that the crack surfaces are often rough [2]. Some of these results are interpreted in the framework of models of cracks propagating in heterogeneous media. The other possibility for the roughening of the crack surfaces is the instability of the straight motion of the crack tip. Recent experiments on the fracture of thin plates [3] clearly established that many puzzling phenomena in brittle fracture dynamics are related to an oscillatory instability at velocities appreciably below the Rayleigh speed VR. Beyond a critical velocity the crack dynamics change dramatically. At that point, the mean acceleration of the crack drops, the crack velocity starts to oscillate, and a pattern correlated with the velocity oscillation is created on the fracture surface. These results stimulated many recent investigations (see, for example, Ref. [4]) but the instability is not well understood yet. There were several attempts in literature to investigate the stability of the propagating cracks. The linear stability analysis of the quasistatic crack subject to mode I (opening-mode) loading has been performed by Cotterell and Rice [5] with subsequent refinement by Adda-Bedia and Ben Amar [6]. They employ the Griffith theory and the so-called principle of local symmetry, i.e., the condition that the mode II (sliding-mode) stress-intensity factor KII vanishes on the tip of the crack. They found that the straight motion of the crack becomes unstable if the tangential loading exceeds a critical value. A fully dynamical model, including the microscopic description of the cohesive zone of the crack tip, has been discussed by Ching, Langer, and Nakanishi [7]. The cohesive force in the neighborhood of the tip provides a fracture energy and a mechanism for regularizing the stress singularity. The use of such a model removes the need to speculate about a principle of local symmetry. In addition to the results of Refs. [5,6], they found a strong microscopic instability even for very low crack velocities. The main reason for such a strong instability is that the tangential stress, which deflects the crack away from a straight motion, exceeds the normal stress on the fracture surface throughout the tip region at all nonzero velocities. This instability is very sensitive to tiny details of the cohesive-zone model. In all of these descriptions, a crack surface is viewed as the trace left behind by the crack tip as it traverses the sample. All modes related to the further surface deformations due to a transfer of matter are assumed to be frozen. The main purpose of this Letter is to describe the instabilities of the crack surface related to these so far missing degrees of freedom. We will find that the surfaces of a propagating crack undergo an Asaro-TillerGrinfeld (ATG) instability [8,9] of purely macroscopic origin.
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