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24 CHAPTER I. FUNDAMENTAL CONCEPTS AND EXAMPLES<br />

to a limit which satisfies the conservation laws (1.1) and the entropy inequality<br />

(3.8). Mild oscillations and spikes are visible near jump discontinuities, only.<br />

Interestingly enough, the limiting solution strongly depends on the parameter<br />

γ. That is, for the same initial data different values of γ lead to different<br />

shock wave solutions !<br />

Ù´Ü Øµ<br />

Ü<br />

Figure I-1 : Numerical solution for<br />

|δ| > ε 2 , respectively.<br />

From this discussion we conclude that no “universal” admissibility criterion can<br />

be postulated for nonlinear hyperbolic systems. Instead, some additional information<br />

should be sought and an admissibility condition should be formulated for each problem<br />

(or rather each class of problems) of interest. Before closing this section let us<br />

introduce a few more properties and definitions. First of all, for the entropy inequality<br />

(3.8) we have the obvious analogue of the Rankine-Hugoniot relation derived earlier<br />

in Section 2.<br />

Theorem 5.1. (Jump relation for the entropy inequality.) We use the same notation<br />

as in Theorem 2.3. The piecewise smooth function (2.7) satisfies the entropy inequality<br />

(3.8) if and only if<br />

−ϕ ′ (t) ( U(u + (t)) − U(u − (t)) ) + F (u + (t)) − F (u − (t)) ≤ 0. (5.2)<br />

In particular, given a shock wave (2.9) connecting two constant states u − and u + and<br />

associated with the speed λ, the entropy inequality reads<br />

−λ ( U(u + ) − U(u − ) ) + F (u + ) − F (u − ) ≤ 0. (5.3)<br />

When dealing with nonclassical solutions, the Rankine-Hugoniot relations (2.10)<br />

and the entropy inequality (5.3) will be supplemented with the following additional<br />

jump condition:<br />

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