{ "id": "0804.3362", "version": "v1", "published": "2008-04-21T17:18:26.000Z", "updated": "2008-04-21T17:18:26.000Z", "title": "q-Gaussians in the porous-medium equation: stability and time evolution", "authors": [ "Veit Schwämmle", "Fernando D. Nobre", "Constantino Tsallis" ], "comment": "20 pages, 6 figures", "doi": "10.1140/epjb/e2008-00451-y", "categories": [ "cond-mat.stat-mech" ], "abstract": "The stability of $q$-Gaussian distributions as particular solutions of the linear diffusion equation and its generalized nonlinear form, $\\pderiv{P(x,t)}{t} = D \\pderiv{^2 [P(x,t)]^{2-q}}{x^2}$, the \\emph{porous-medium equation}, is investigated through both numerical and analytical approaches. It is shown that an \\emph{initial} $q$-Gaussian, characterized by an index $q_i$, approaches the \\emph{final}, asymptotic solution, characterized by an index $q$, in such a way that the relaxation rule for the kurtosis evolves in time according to a $q$-exponential, with a \\emph{relaxation} index $q_{\\rm rel} \\equiv q_{\\rm rel}(q)$. In some cases, particularly when one attempts to transform an infinite-variance distribution ($q_i \\ge 5/3$) into a finite-variance one ($q<5/3$), the relaxation towards the asymptotic solution may occur very slowly in time. This fact might shed some light on the slow relaxation, for some long-range-interacting many-body Hamiltonian systems, from long-standing quasi-stationary states to the ultimate thermal equilibrium state.", "revisions": [ { "version": "v1", "updated": "2008-04-21T17:18:26.000Z" } ], "analyses": { "subjects": [ "05.40.Fb", "05.20.-y", "05.40.Jc" ], "keywords": [ "time evolution", "porous-medium equation", "ultimate thermal equilibrium state", "asymptotic solution", "q-gaussians" ], "tags": [ "journal article" ], "publication": { "journal": "European Physical Journal B", "year": 2008, "month": "Dec", "volume": 66, "number": 4, "pages": 537 }, "note": { "typesetting": "TeX", "pages": 20, "language": "en", "license": "arXiv", "status": "editable", "adsabs": "2008EPJB...66..537S" } } }