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Dissipative function

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dissipation function

A function used to take into account the effect of the forces of viscous friction on the motion of a mechanical system. The dissipation function describes the rate of decrease of the mechanical energy of the system; it is also used, more generally, to allow for the transition of energy of ordered motion to energy of disordered motion (ultimately to thermal energy).

The dissipation function for an isotropic medium, referred to unit volume, has the form

where are the components of the tensor of the deformation rates and and are the viscosity coefficients which describe the viscosity during motion and the viscosity during volume expansion, respectively.

The equation of change of entropy in a viscous medium has the form:

where is the specific entropy, is the density and is the temperature of the liquid.

The dissipation function is a characterization of the viscous forces during the motion of a continuous medium. The equation of motion of a viscous medium is

where the are the components of the friction-less part of the stress tensor, the

are the components of the "viscous" part of the stress tensor, and

The dissipation function is employed to allow for the effect of the resistance to small vibrations of the system around its equilibrium position; to study the damping of vibrations in an elastic medium; to allow for heat losses during the damping of electric current vibrations in circuit systems; etc.

References

[1] L.D. Landau, E.M. Lifshitz, "Fluid mechanics" , Pergamon (1959) (Translated from Russian)


Comments

For a Newtonian fluid the stress tensor has components , where is the friction-less part (above called ) and is the viscous part.

References

[a1] S.J. Pai, "Viscous flow theory" , 1. Laminar flow , v. Nostrand (1956)
How to Cite This Entry:
Dissipative function. Encyclopedia of Mathematics. URL: http://encyclopediaofmath.org/index.php?title=Dissipative_function&oldid=15366
This article was adapted from an original article by V.A. Dorodnitsyn (originator), which appeared in Encyclopedia of Mathematics - ISBN 1402006098. See original article