THE THERMODYNAMIC DESCRIPTION OF HETEROGENEOUS DISSIPATIVE SYSTEMS BY VARIATIONAL METHODS: IV. CONSEQUENCES OF A SYNTHESIS OF THE ONSAGER AND PRIGOGINE PRINCIPLES

1964 ◽  
Vol 42 (8) ◽  
pp. 1447-1454 ◽  
Author(s):  
J. S. Kirkaldy

Since Onsager's steady-state dissipation principle and Prigogine's principle of minimum entropy production share a common Euler–Lagrange equation, their configuration spaces may be combined to form a single potential surface. As applied to phase transformations, the entropy production forms a saddle surface in the configuration space of possible stationary states. Those macroscopic variations which involve a change in morphology and a corresponding change in the thermodynamic forces during a spontaneous regression stabilize at a minimum of the entropy production (Prigogine's principle), whereas those microscopic variations, due to fluctuations of the fluxes with fixed forces and fixed morphology, stabilize at a maximum of the entropy production (Onsager's principle). A stable steady state is, therefore, defined by the saddle point.The internal constraints attending stationary phase transformation often exclude the saddle point as a possible state so that unstable configurations are obtained. Dendritic growth of alloy crystals is an example.Some isothermal eutectic or eutectoid reactions may be located at the saddle point. In this case the stabilization of the configuration against microscopic fluctuations requires that the reaction product be in metastable equilibrium. Alteration of the growth conditions may lead to macroscopic instability and a transition to a state lying off the saddle point. These systems evidence their instability by the roughly periodic form of the reaction products.

1964 ◽  
Vol 42 (8) ◽  
pp. 1437-1446 ◽  
Author(s):  
J. S. Kirkaldy

The stable free-fall flight of a maple seed gives an exceptionally graphic demonstration of the principle of minimum entropy production. Since the rate of entropy production is proportional to the steady-state rate of loss of potential energy, it is visually obvious that the stable rotary configuration represents a minimum of the entropy production rate relative to an unstable steady-state bomblike trajectory. Regarding this phenomenon as the prototype of many practical steady-state fluid-dynamical systems involving rotational modes, we formally demonstrate the possibility of mathematically defining the stable steady-state configuration by means of this variational principle.


2012 ◽  
Vol 560-561 ◽  
pp. 140-144
Author(s):  
Yuan Zhen Cai

Based on the irreversible thermodynamics, a irreversible thermodynamic description of domain occurrences in ferroics such as ferroelectrics, ferromagnetics and ferroelastics was given. The ferroic domain structures occur at the ferroic phase transitions from the prototype phases to the ferroic phases. The processes of transition are stationary state processes so that the principle of minimum entropy production is satisfied. The domain occurrences are a consequence of this principle. The time-spatial symmetry related to the domains and their occurrences was also expounded.


2005 ◽  
Vol 51 (172) ◽  
pp. 125-138 ◽  
Author(s):  
Perry Bartelt ◽  
Othmar Buser ◽  
Martin Kern

AbstractWe derive work dissipation functionals for granular snow avalanches flowing in simple shear. Our intent is to apply constructive theorems of non-equilibrium thermodynamics to the snow avalanche problem. Snow chute experiments show that a bi-layer system consisting of a non-yielded flow plug overriding a sheared fluidized layer can be used to model avalanche flow. We show that for this type of constitutive behaviour the dissipation functionals are minimum at steady state with respect to variations in internal velocity; however, the functionals must be constrained by subsidiary mass- continuity integrals before the equivalence of momentum balance and minimal work dissipation can be established. Constitutive models that do not satisfy this equivalence are henceforth excluded from our consideration. Fluctuations in plug and slip velocity depend on the roughness of the flow surface and viscosity of the granular system. We speculate that this property explains the transition from flowing avalanches to powder avalanches. Because the temperature can safely be assumed constant, we demonstrate within the context of non-equilibrium thermodynamics that granular snow avalanches are irreversible, dissipative systems, minimizing – in space – entropy production. Furthermore, entropy production is linear both near and far from steady-state non-equilibrium because of the mass-continuity constraint. Finally, we derive thermodynamic forces and conjugate fluxes as well as expressing the corresponding phenomenological Onsager coefficients in terms of the constitutive parameters.


Entropy ◽  
2018 ◽  
Vol 20 (11) ◽  
pp. 811 ◽  
Author(s):  
Miguel Pineda ◽  
Michail Stamatakis

Catalytic surface reaction networks exhibit nonlinear dissipative phenomena, such as bistability. Macroscopic rate law descriptions predict that the reaction system resides on one of the two steady-state branches of the bistable region for an indefinite period of time. However, the smaller the catalytic surface, the greater the influence of coverage fluctuations, given that their amplitude normally scales as the square root of the system size. Thus, one can observe fluctuation-induced transitions between the steady-states. In this work, a model for the bistable catalytic CO oxidation on small surfaces is studied. After a brief introduction of the average stochastic modelling framework and its corresponding deterministic limit, we discuss the non-equilibrium conditions necessary for bistability. The entropy production rate, an important thermodynamic quantity measuring dissipation in a system, is compared across the two approaches. We conclude that, in our catalytic model, the most favorable non-equilibrium steady state is not necessary the state with the maximum or minimum entropy production rate.


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