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@ARTICLE{Barras:873491,
      author       = {Barras, Fabian and Aldam, Michael and Roch, Thibault and
                      Brener, Efim A. and Bouchbinder, Eran and Molinari,
                      Jean-François},
      title        = {{E}mergence of {C}racklike {B}ehavior of {F}rictional
                      {R}upture: {T}he {O}rigin of {S}tress {D}rops},
      journal      = {Physical review / X Expanding access X},
      volume       = {9},
      number       = {4},
      issn         = {2160-3308},
      address      = {College Park, Md.},
      publisher    = {APS},
      reportid     = {FZJ-2020-00768},
      pages        = {041043},
      year         = {2019},
      abstract     = {The process of frictional rupture, i.e., the failure of
                      frictional systems, abounds in the technological and natural
                      world around us, ranging from squealing car brake pads to
                      earthquakes along geological faults. A general framework for
                      understanding and interpreting frictional rupture commonly
                      involves an analogy to ordinary crack propagation, with
                      far-reaching implications for various disciplines from
                      engineering tribology to geophysics. An important feature of
                      the analogy to cracks is the existence of a reduction in the
                      stress-bearing capacity of the ruptured interface, i.e., of
                      a drop from the applied stress, realized far ahead of a
                      propagating rupture, to the residual stress left behind it.
                      Yet, how and under what conditions such finite and
                      well-defined stress drops emerge from basic physics are not
                      well understood. Here, we show that for a rapid rupture a
                      stress drop is directly related to wave radiation from the
                      frictional interface to the bodies surrounding it and to
                      long-range bulk elastodynamics and not exclusively to the
                      physics of the contact interface. Furthermore, we show that
                      the emergence of a stress drop is a transient effect,
                      affected by the wave travel time in finite systems and by
                      the decay of long-range elastic interactions. Finally, we
                      supplement our results for rapid rupture with predictions
                      for a slow rupture. All of the theoretical predictions are
                      supported by available experimental data and by extensive
                      computations. Our findings elucidate the origin of stress
                      drops in frictional rupture; i.e., they offer a
                      comprehensive and fundamental understanding of why, how, and
                      to what extent frictional rupture might be viewed as an
                      ordinary fracture process.},
      cin          = {PGI-2},
      ddc          = {530},
      cid          = {I:(DE-Juel1)PGI-2-20110106},
      pnm          = {144 - Controlling Collective States (POF3-144)},
      pid          = {G:(DE-HGF)POF3-144},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000498884000002},
      doi          = {10.1103/PhysRevX.9.041043},
      url          = {https://juser.fz-juelich.de/record/873491},
}