defray 发表于 2025-3-25 04:31:52
Martijn A. Boermans,Hein Roelfsemadent variables, through the introduction of non-equilibrium variables, such as the dissipative fluxes appearing in the balance equations. The next step is to find evolution equations for these extra variables. Whereas the evolution equations for the classical variables are given by the usual balancepaltry 发表于 2025-3-25 10:37:51
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Introduction: The IMPETUS methode shall present many illustrations of how these equations are useful in interpreting experimental data or dealing with situations which are beyond the scope of the classical theory. In this chapter, our interest is focused on the generalized Gibbs equation, which is the central thermodynamic resultWITH 发表于 2025-3-25 18:28:41
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https://doi.org/10.1007/978-3-540-37224-0the introduction of supplementary boundary and initial conditions compared to classical thermo-hydrodynamics. However, instead of trying to solve the whole mathematical problem, it is more fruitful to concentrate on the analysis of waves, which is, furthermore, a situation of great experimental inteornithology 发表于 2025-3-26 09:12:20
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https://doi.org/10.1007/978-3-030-71073-6umstances the classical Fick law gives an excellent description, it appears insufficient for describing some particular features, like those concerned with relaxational effects; they are of importance in many different applications which have been studied in the framework of stochastic processes as注视 发表于 2025-3-26 18:45:11
https://doi.org/10.1007/978-3-642-54919-9cularly interesting situation, that of systems under shear flow. The presence of a non-vanishing shear results in drastic changes in the phase diagram of the system and in chemical reactions taking place within it. We shall illustrate our analysis by considering polymer solutions, wherein significan