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Luc TARTAR Compensated Compactness with more ... - ICMS

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I was puzzled that they considered a not so realistic EOS (equation<br />

of state), since incompressibility implies an infinite speed<br />

of sound, <strong>with</strong>out saying what to do for a realistic situation,<br />

of a (compressible) fluid occupying a domain Ω ⊂ R 3 having a<br />

boundary (while compact manifolds have no boundary)!<br />

Thirty years after I was again puzzled that for writing the<br />

questions for the million dollar Clay Prize on Navier–Stokes<br />

equation, Charles FEFFERMAN could not find (in Princeton<br />

or elsewhere) a knowledgeable person (mathematician or not)<br />

who could tell him what the equation is about: he should have<br />

mentioned the basic conservation laws of Continuum Mechanics<br />

and explained why he did not use the conservation of energy;<br />

among the groups of invariance of the equation he should have<br />

mentioned the invariance by rotation (since one considers an<br />

isotropic fluid) and Galilean invariance; in selecting cases <strong>with</strong>out<br />

boundary (R 3 or a flat torus) he should have mentioned<br />

that realistic domains have a boundary, and because bounding<br />

the vorticity is the main difficulty for proving global existence<br />

of smooth solutions, he should have mentioned the importance<br />

of the boundary, since it seems that vorticity is created there.<br />

In 1970, I first read about covariant derivatives, used for writing<br />

Navier–Stokes equation on a Riemannian manifold, but<br />

later I wondered why geometers think it is a good way to<br />

write such equations: is their framework useful for <strong>more</strong> general<br />

EOS For example, realistic fluids have their viscosity depending<br />

upon temperature, maybe also upon pressure.<br />

Geometers (and later harmonic analysts) seemed to think that<br />

they were doing a useful job in writing equations of Continuum<br />

Mechanics in their language, but has it led to a natural way of<br />

obtaining a priori estimates for flows of realistic fluids<br />

4

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