Journal
COMPTES RENDUS MATHEMATIQUE
Volume 354, Issue 5, Pages 503-509Publisher
ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER
DOI: 10.1016/j.crma.2016.02.008
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Funding
- NSF (USA) [1255622]
- CAPES(Brazil) [88881.067966/2014-01]
- Division Of Earth Sciences
- Directorate For Geosciences [1255622] Funding Source: National Science Foundation
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In a seminal work in 1934, J. Leray constructed solutions u(., t) is an element of L-infinity([0, infinity), L-alpha(2)(R-3)) boolean AND C-w(0)([0, infinity), L-2(R-3)) boolean AND L-2([0, infinity), (H) over dot(1)(R-3)) of the Navier-Stokes equations for arbitrary initial data u(., 0). L-sigma(2)(R-3) and left it open whether parallel to u(., t)parallel to(L2(R3)) would necessarily tend to zero as t -> infinity. This question was answered positively fifty years later by T. Kato, using a different approach. Here, we reexamine Leray's problem and solve this and other important related questions using Leray's original ideas and some standard tools (Fourier transform, Duhamel's principle, heat kernel estimates) already in use in his time. (C) 2016 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.
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