Gradient structures and geodesic convexity for reaction–diffusion systems
2013 ◽
Vol 371
(2005)
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pp. 20120346
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Keyword(s):
We consider systems of reaction–diffusion equations as gradient systems with respect to an entropy functional and a dissipation metric given in terms of a so-called Onsager operator, which is a sum of a diffusion part of Wasserstein type and a reaction part. We provide methods for establishing geodesic λ -convexity of the entropy functional by purely differential methods, thus circumventing arguments from mass transportation. Finally, several examples, including a drift–diffusion system, provide a survey on the applicability of the theory.
2003 ◽
Vol 189
(1)
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pp. 130-158
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pp. 1163-1182
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pp. 265-286
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pp. 1903-1917
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pp. 1417-1423
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pp. 1149-1158
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Vol 61
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pp. 59-78
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