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Bilateral propagation of a spontaneous two‐dimensional anti‐plane shear crack under the influence of cohesion
Author(s) -
Chatterjee A. K.,
Knopoff L.
Publication year - 1983
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1983.tb03324.x
Subject(s) - cohesion (chemistry) , mechanics , shear (geology) , drop (telecommunication) , fissure , slip (aerodynamics) , fracture mechanics , crack closure , materials science , physics , composite material , engineering , telecommunications , quantum mechanics , thermodynamics
Summary. We consider the problem of the bilateral extension of a two‐dimensional anti‐plane shear crack that initiates spontaneously at a point and extends under the influence of cohesive forces at the edges. An approximation to the stresses in the regions beyond the edges of the crack has been found that simplifies the calculation. The exact stresses in these regions are also found iteratively. In the cases of uniformly propagating cracks, the estimates of cohesive forces obtained from the approximation are close to the exact values for high crack speeds but are significantly different for low crack speeds. It is also found that if healing is initiated due to the encounter of one end of a uniformly propagating crack with an unbreakable barrier, the static stress drop in the torn region is constant but may either overshoot or undershoot the dynamical stress drop. In these cases, the final static slip distribution is obtained by freezing the dynamic solution along a characteristic line through the location of the barrier. We find that the crack length cannot be unambiguously derived from the far field spectral properties.

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