Physics of Geological Processes, University of Oslo, Norway.
Phys Rev Lett. 2011 Aug 12;107(7):074301. doi: 10.1103/PhysRevLett.107.074301.
We describe a 2D spring-block model for the transition from static to kinetic friction at an elastic-slider-rigid-substrate interface obeying a minimalistic friction law (Amontons-Coulomb). By using realistic boundary conditions, a number of previously unexplained experimental results on precursory microslip fronts are successfully reproduced. From the analysis of the interfacial stresses, we derive a prediction for the evolution of the precursor length as a function of the applied loads, as well as an approximate relationship between microscopic and macroscopic friction coefficients. We show that the stress buildup due to both elastic loading and microslip-related relaxations depends only weakly on the underlying shear crack propagation dynamics. Conversely, crack speed depends strongly on both the instantaneous stresses and the friction coefficients, through a nontrivial scaling parameter.
我们描述了一个二维弹簧块模型,用于模拟在遵循简化摩擦定律(阿蒙顿-库仑定律)的弹性滑块-刚性基底界面上,从静摩擦到动摩擦的转变。通过使用现实的边界条件,我们成功地再现了许多以前无法解释的关于预滑微滑前导的实验结果。从界面应力分析中,我们推导出了作为外加负载函数的前导长度的演化预测,以及微观和宏观摩擦系数之间的近似关系。我们表明,由于弹性加载和与微滑相关的松弛引起的应力积累仅与基础剪切裂纹扩展动力学的弱相关。相反,裂纹速度强烈依赖于瞬时应力和摩擦系数,通过一个非平凡的比例参数。