Citation:
Mier, J.A., Sánchez, R., & Newman, D. E. 2020. Tracer particle transport dynamics in the diffusive sandpile cellular automaton. In Chaos, Solitons & Fractals, 140, 110117-110126
xmlui.dri2xhtml.METS-1.0.item-contributor-funder:
Ministerio de Economía y Competitividad (España) Universidad Carlos III de Madrid
Sponsor:
This research has been sponsored in part by Ministerio de
Economía y Competitividad of Spain under Projects No. ENE2015-
68265-P and No. ENE2015-66444-R. Research also supported in
part by DOE-OFES Grant No. DE-FG02-04ER5741 at University of
Alaska. Sandpile simulations have been run in Uranus, a supercomputer cluster at Universidad Carlos III de Madrid (Spain) that
has been funded by the Spanish Government via the national
projects UNC313-4E-2361, ENE2009-12213-C03-03, ENE2012-33219
and ENE2012-31753.
Project:
Gobierno de España. ENE2009-12213-C03-03 Gobierno de España. ENE2012-33219 Gobierno de España. ENE2012-31753 Indefinido. UNC313-4E-2361 Gobierno de España. ENE2015-68265-P Gobierno de España. ENE2015-66444-R
The confinement properties of the diffusive running sandpile are characterized by tracking the motion of a population of marked grains of sand. It is found that, as the relative strength of the avalanching to the diffusive transport channel is varied, a point The confinement properties of the diffusive running sandpile are characterized by tracking the motion of a population of marked grains of sand. It is found that, as the relative strength of the avalanching to the diffusive transport channel is varied, a point is reached at which the particle global confinement time and the probability density functions of the jump-sizes and waiting-times of the tracked grains experience a sudden change, thus revealing a dynamical transition, that is consistent with previous studies (Newman DE et al., Phys Rev Lett 2002;88(20):204304). Across this transition, the sandpile moves from a regime characterized by self-similarity and memory, where avalanches of all possible sizes dominate transport across the system, to another regime where transport is taken over by near system-size, quasi-periodic avalanches. Values for the fractional transport exponents that quantify effective transport across the sandpile prior to the transition are also obtained.[+][-]