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Titlebook: Extended Irreversible Thermodynamics; David Jou,José Casas-Vázquez,Georgy Lebon Book 19931st edition Springer-Verlag Berlin Heidelberg 199

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发表于 2025-3-21 18:10:29 | 显示全部楼层 |阅读模式
书目名称Extended Irreversible Thermodynamics
编辑David Jou,José Casas-Vázquez,Georgy Lebon
视频video
图书封面Titlebook: Extended Irreversible Thermodynamics;  David Jou,José Casas-Vázquez,Georgy Lebon Book 19931st edition Springer-Verlag Berlin Heidelberg 199
描述Classical irreversible thermodynamics, as developed by Onsager, Prigogine and many other authors, is based on the local-equilibrium hypothesis. Out of equilibrium, any system is assumed to depend locally on the same set of variables as when it is in eqUilibrium. This leads to a formal thermody­ namic structure identical to that of eqUilibrium: intensive parameters such as temperature, pressure and chemical potentials are well-defined quantities keeping their usual meaning, thermodynamic potentials are derived as Leg­ endre transformations and all equilibrium thermodynamic relations retain their validity. The theory based on this hypothesis has turned out to be very useful and has achieved a number of successes in many practical situations. of interest in going However, the recent decade has witnessed a surge beyond the classical formulation. There are several reasons for this. One of them is the development of experimental methods able to deal with the response of systems to high-frequency and short-wavelength perturbations, such as ultrasound propagation and light and neutron scattering. The ob­ served results have led to generalizations of the classical hydrodynamical theories, b
出版日期Book 19931st edition
关键词Polymere; condensed matter; irreversible Thermodynamik; irreversible thermodynamics; kinetic theory; none
版次1
doihttps://doi.org/10.1007/978-3-642-97430-4
isbn_ebook978-3-642-97430-4
copyrightSpringer-Verlag Berlin Heidelberg 1993
The information of publication is updating

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Climate Change and Climate Models,p is to find evolution equations for the dissipative fluxes. Whereas the evolution equations for the classical variables are given by the usual balance laws, no general criteria exist concerning the evolution equations of the dissipative fluxes, with the exception of the restrictions imposed on them by the second law of thermodynamics.
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https://doi.org/10.1007/978-3-030-11172-4ur interest is focused on the generalized Gibbs equation, which is the central thermodynamic result of extended irreversible thermodynamics. Our aim is to show that the generalized entropy plays an essential role in the description of the fluctuations around equilibrium states of not only the conserved variables but the dissipative fluxes, too.
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Book 19931st edition equilibrium, any system is assumed to depend locally on the same set of variables as when it is in eqUilibrium. This leads to a formal thermody­ namic structure identical to that of eqUilibrium: intensive parameters such as temperature, pressure and chemical potentials are well-defined quantities k
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Extended Irreversible Thermodynamicsp is to find evolution equations for the dissipative fluxes. Whereas the evolution equations for the classical variables are given by the usual balance laws, no general criteria exist concerning the evolution equations of the dissipative fluxes, with the exception of the restrictions imposed on them by the second law of thermodynamics.
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