Record Dynamics: Direct Experimental Evidence from Jammed Colloids
arXiv:1608.03869 · doi:10.1209/0295-5075/116/38003
Abstract
In a broad class of complex materials a quench leads to a multi-scaled relaxation process known as aging. To explain its commonality and the astounding insensitivity to most microscopic details, record dynamics (RD) posits that a small set of increasingly rare and irreversible events, so called quakes, controls the dynamics. While key predictions of RD are known to concur with a number of experimental and simulational results, its basic assumption on the nature of quake statistics has proven extremely difficult to verify experimentally. The careful distinction of rare ("record") cage-breaking events from in-cage rattle accomplished in previous experiments on jammed colloids, enables us to extract the first direct experimental evidence for the fundamental hypothesis of RD that the rate of quakes decelerates with the inverse of the system age. The resulting description shows the predicted growth of the particle mean square displacement and of a mesoscopic lengthscale with the logarithm of time.
6 pages, RevTex, changed title, many updates and corrections; for related information, see http://www.physics.emory.edu/faculty/boettcher/
References in corpus (6)
- Dynamic heterogeneity in amorphous materials
- Evolution in complex systems
- Record dynamics and the observed temperature plateau in the magnetic creep rate of type II superconductors
- Subdiffusion and intermittent dynamic fluctuations in the aging regime of concentrated hard spheres
- Intermittency, aging and record fluctuations
- Aging and intermittency in a p-spin model of a glass