Pressure shock fronts formed by ultra-fast shear cracks in viscoelastic materials.

Pressure shock fronts formed by ultra-fast shear cracks in viscoelastic materials.
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DOI:
10.1038/s41467-018-07139-4
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发表时间:
2018-11-12
影响因子:
16.6
通讯作者:
Lapusta N
Lapusta N
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Gori M;Rubino V;Rosakis AJ;Lapusta N

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Spontaneously propagating cracks in solids emit both pressure and shear waves. When a shear crack propagates faster than the shear wave speed of the material, the coalescence of the shear wavelets emitted by the near-crack-tip region forms a shock front that significantly concentrates particle motion. Such a shock front should not be possible for pressure waves, because cracks should not be able to exceed the pressure wave speed in isotropic linear-elastic solids. In this study, we present full-field experimental measurements of dynamic shear cracks in viscoelastic polymers that result in the formation of a pressure shock front, in addition to the shear one. The apparent violation of classic theories is explained by the strain-rate-dependent material behavior of polymers, where the crack speed remains below the highest pressure wave speed prevailing locally around the crack tip. These findings have important implications for the physics and dynamics of shear cracks such as earthquakes. Propagating shear cracks in solids emit both shear and pressure waves, but it is usually thought that only shear waves coalesce to form shock fronts when the crack exceeds the shear wave speed. Here, the authors show that local material stiffening can further increase rupture speed and produce pressure shock fronts that hint at supersonic propagation.
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