Download The Porous Medium Equation: Mathematical Theory by Juan Luis Vazquez PDF

By Juan Luis Vazquez

The warmth Equation is without doubt one of the 3 classical linear partial differential equations of moment order that shape the root of any undemanding creation to the world of PDEs, and just recently has it turn out to be relatively good understood. during this monograph, aimed toward learn scholars and lecturers in arithmetic and engineering, in addition to engineering experts, Professor Vazquez offers a scientific and finished presentation of the mathematical conception of the nonlinear warmth equation frequently referred to as the Porous Medium Equation (PME). This equation appears to be like in a few actual purposes, comparable to to explain strategies regarding fluid circulate, warmth move or diffusion. different functions were proposed in mathematical biology, lubrication, boundary layer concept, and different fields. every one bankruptcy incorporates a specific creation and is provided with a piece of notes, delivering reviews, historic notes or instructed interpreting, and routines for the reader.

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A further extension is the generalized porous medium equation, ∂t u = ∆Φ(u) + f, (GPME) also called the filtration equation, specially in the Russian literature; Φ is an increasing function: R+ → R+ , and usually f = 0. The diffusion coefficient is now D(u) = Φ (u), and the condition Φ (u) ≥ 0 is needed to make the equation formally parabolic. Whenever Φ (u) = 0 for some u ∈ R, we say that the equation 8 Introduction degenerates at that u-level, since it ceases to be strictly parabolic. This is the cause for more or less serious departures from the standard quasilinear theory, as we have already explained in the PME case.

Even if f = 0 we can get estimates. 3. An interesting particular case happens when j(s) = |s|r for some r > 1. When f = 0 we get monotonicity of the Lr norm d dt |u(t)|r dx ≤ 0. In case Φ depends on x, we above argument does not work because of the derivatives of Φ(x, z) with respect to x. We refrain from entering into the modifications which are not at immediate. 3 The stability estimate. L1 contraction This is a very important estimate which has played a key role in the PME and the GPME theory.

1 Quasilinear equations and the PME Let us review the properties of the solutions to quasilinear parabolic problems of the form d ∂t u = i=1 ∂ ai (x, t, u, ∇u) + b(x, t, u, ∇u). 1) where ai (x, t, u, p1 , . . , pd ) and b(x, t, u, p1 , . . , pd ) are called structural functions. They must satisfy certain conditions to ensure that a theory including existence, uniqueness and a certain regularity can be developed. The main condition is parabolicity to be explained presently. We will follow Ladyzhenskaya et al.

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