“…In solids, granular materials and structures, the effect is a transientinduced disequilibrium, where the material modulus decreases and the dissipation increases, and which may become permanent if deformations are large or frequent. Materials also commonly exhibit a fascinating, slow dynamical recovery from disequilibrium to the original or a new equilibrium of the system's elastic properties after strong wave deformations terminate, observed in the laboratory on rocks (e.g., Guyer and Johnson, 1999;Johnson and Sutin, 2005;TenCate, 2011;Renaud et al, 2012;Renaud et al, 2014), in concrete materials (e.g., Lacouture et al, 2003;Bentahar et al, 2006;Bui et al, 2013), at the Earth's surface in soils (e.g., Field et al, 1997;Sawazaki et al, 2009;Wu et al, 2009a;Ohmachi and Tahara, 2011;Johnson et al, 2009;Renaud et al, 2014) and at the scale of the Earth's crust (Peng and Ben-Zion, 2006;Karabulut and Bouchon, 2007;Brenguier et al, 2008;Wu et al, 2009b). Between laboratory and crustal scales, we studied an intermediate scale system: a civil engineering structure.…”