By Ansgar Jüngel

ISBN-10: 3319342185

ISBN-13: 9783319342184

ISBN-10: 3319342193

ISBN-13: 9783319342191

This booklet offers quite a number entropy equipment for diffusive PDEs devised by means of many researchers throughout the previous few a long time, which permit us to appreciate the qualitative habit of suggestions to diffusive equations (and Markov diffusion processes). functions comprise the large-time asymptotics of suggestions, the derivation of convex Sobolev inequalities, the life and distinctiveness of vulnerable options, and the research of discrete and geometric constructions of the PDEs. the aim of the ebook is to supply readers an advent to chose entropy equipment that may be present in the examine literature. with the intention to spotlight the middle recommendations, the implications usually are not said within the widest generality and many of the arguments are just formal (in the experience that the practical environment isn't distinctive or enough regularity is supposed). The textual content can be compatible for complex grasp and PhD scholars and will function a textbook for distinctive classes and seminars.

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**Extra info for Entropy Methods for Diffusive Partial Differential Equations**

**Example text**

J. Math. Phys. 25, 3120–3123 (1984) 36. : The geometry of dissipative evolution equations: the porous medium equation. Commun. Part. Diff. Equ. 26, 101–174 (2001) 37. : A Lyapunov functional for the evolution of solutions to the porous medium equation to self-similarity II. J. Math. Phys. 25, 3124–3127 (1984) 38. : Methods of Modern Mathematical Physics. Analysis of Operators, vol. 4. Academic Press, San Diego (1978) 39. : The Fokker–Planck Equation. Methods of Solution and Applications, 2nd edn.

The calculations can be justified by a suitable approximation procedure. 3) consists in the following identity: Pα [u] = − T u α+β−2 u x x x u x dx = (α + β − 2) T u α+β−3 u 2x u x x dx + T u α+β−2 u 2x x dx. 2 The One-Dimensional Case 47 The last equation can be written equivalently as I2 = = T ux u u α+β (α + β − 2) u α+β T ux uxx u u x 2 uxx uxx + u u 2 + ux uxxx dx u u dx = 0. The integral vanishes because of the periodic boundary conditions. 4) can be written as Pα [u] = Pα [u] + c · I2 with c = 1.

Hence, there exists a f ∗ weakly in H 1 ( ) as k → ∞. subsequence (not relabeled) such that f (u(tk ))) ∞ Since (u(tk )) is bounded in L ( ), we also have f (u(tk )) → f (u ∗ ) strongly in L 2 ( ). Thus, we can identify the limit, f ∗ = f (u ∗ ). The convergences u(tk ) → f (u ∗ ) weakly in H 1 ( ) allow us to deduce u ∗ uniformly in and f (u(tk )) ∗ that u = u ∞ (this step requires some effort). Then the convergence u(tk ) → u ∞ uniformly in is sufficient to conclude that limk→∞ H∗ [u(tk )] = H∗ [u ∞ ] = 0.

### Entropy Methods for Diffusive Partial Differential Equations by Ansgar Jüngel

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