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- W4312132301 abstract "Friction resisting sliding over contacted surfaces of faults or shear fractures is usually considered independent of the sliding direction. However, when the rock near sliding surface is anisotropic with a symmetry axis inclined to the sliding direction, normal constraint induces asymmetry, whereby friction forces resisting sliding in opposite directions are different. In this case the applied oscillatory force produces sliding towards the direction with the smallest friction such that macroscopic movement can occur even when the driving force oscillates around zero. Furthermore, friction asymmetry leads to emerging of a critical value of friction in the hard direction: for friction forces lower than the critical value the exponent of the fall-off of the velocity power spectra is near the conventional −1, while when the friction force reaches the critical value the exponent drops to −2. This phenomenon can be used for reconstructing the structure of rocks surrounding sliding fractures/faults." @default.
- W4312132301 created "2023-01-04" @default.
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- W4312132301 date "2022-12-13" @default.
- W4312132301 modified "2023-09-28" @default.
- W4312132301 title "Anomalous Fall-Off in Velocity Power Spectra Caused by Sliding with Asymmetric Friction" @default.
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- W4312132301 doi "https://doi.org/10.1007/978-3-031-22213-9_19" @default.
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