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Universal scaling in transient creep
Authors:Dysthe Dag Kristian  Podladchikov Yuri  Renard Francois  Feder Jens  Jamtveit Bjørn
Institution:Physics of Geological Processes, Postbox 1048 Blindern, N-0316 Oslo, Norway. d.k.dysthe@fys.uio.no
Abstract:We present experimental evidence that pressure solution creep does not establish a steady-state interface microstructure as previously thought. Conversely, pressure solution controlled strain and the characteristic length scale of interface microstructures grow as the cubic root of time. Transient creep with the same scaling is known in metallurgy (Andrade creep). The apparent universal scaling of pressure solution transient creep is explained using an analogy with spinodal dewetting.
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