Viscous force: Difference between revisions

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<div class="definition"><div class="short_definition">The force per unit volume or per unit mass arising from the action of [[tangential  stresses]] in a moving [[viscous fluid]]; this force may then be introduced as a term in the [[equations  of motion]].</div><br/> <div class="paragraph">By far the most satisfactory hypothesis to date is that of Navier and Stokes, a generalization of  the [[Newtonian friction law]], which evaluates the [[stress tensor]] as directly proportional to the rate  of [[deformation]], the constant of proportionality being the [[dynamic viscosity]]. In this case, the  viscous force per unit mass becomes  <div class="display-formula"><blockquote>[[File:ams2001glos-Ve15.gif|link=|center|ams2001glos-Ve15]]</blockquote></div> where &#x003bd; is the [[kinematic viscosity]], '''V''' the [[velocity]] vector, and '''&nabla;''' the [[del operator]]. The [[divergence]]  term, '''&nabla;'''&middot;'''V''', vanishes for an [[incompressible fluid]], and the Navier&ndash;Stokes assumption is seen as  leading to a simple [[diffusion]] of [[momentum]]. "It may seem a little strange that [[viscosity]], which  is a diffusion of momentum, can also diffuse [[energy]] and even [[Reynolds stresses]]. . . . A viscous  [[stress]] acts both to convert mechanical [[energy]] into [[heat]] and to accelerate neighboring fluid, and  this [[acceleration]] is an [[energy transfer]]. . . ." (Townsend 1956). <br/>''See'' [[Navier&ndash;Stokes equations]].</div><br/> </div><div class="reference">Townsend, A. A. 1956. The Structure of Turbulent Shear Flow.  Cambridge University Press, . p. 30. </div><br/>  
<div class="definition"><div class="short_definition">The force per unit volume or per unit mass arising from the action of [[tangential stresses|tangential  stresses]] in a moving [[viscous fluid]]; this force may then be introduced as a term in the [[equations of motion|equations  of motion]].</div><br/> <div class="paragraph">By far the most satisfactory hypothesis to date is that of Navier and Stokes, a generalization of  the [[Newtonian friction law]], which evaluates the [[stress tensor]] as directly proportional to the rate  of [[deformation]], the constant of proportionality being the [[dynamic viscosity]]. In this case, the  viscous force per unit mass becomes  <div class="display-formula"><blockquote>[[File:ams2001glos-Ve15.gif|link=|center|ams2001glos-Ve15]]</blockquote></div> where &#x003bd; is the [[kinematic  viscosity|kinematic viscosity]], '''V''' the [[velocity]] vector, and '''&nabla;''' the [[del operator]]. The [[divergence]]  term, '''&nabla;'''&middot;'''V''', vanishes for an [[incompressible fluid]], and the Navier&ndash;Stokes assumption is seen as  leading to a simple [[diffusion]] of [[momentum]]. "It may seem a little strange that [[viscosity]], which  is a diffusion of momentum, can also diffuse [[energy]] and even [[Reynolds stresses]]. . . . A viscous  [[stress]] acts both to convert mechanical [[energy]] into [[heat]] and to accelerate neighboring fluid, and  this [[acceleration]] is an [[energy transfer]]. . . ." (Townsend 1956). <br/>''See'' [[Navier&ndash;Stokes equations]].</div><br/> </div><div class="reference">Townsend, A. A. 1956. The Structure of Turbulent Shear Flow.  Cambridge University Press, . p. 30. </div><br/>  
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Latest revision as of 17:12, 25 April 2012



viscous force

The force per unit volume or per unit mass arising from the action of tangential stresses in a moving viscous fluid; this force may then be introduced as a term in the equations of motion.

By far the most satisfactory hypothesis to date is that of Navier and Stokes, a generalization of the Newtonian friction law, which evaluates the stress tensor as directly proportional to the rate of deformation, the constant of proportionality being the dynamic viscosity. In this case, the viscous force per unit mass becomes
ams2001glos-Ve15
where ν is the kinematic viscosity, V the velocity vector, and the del operator. The divergence term, ·V, vanishes for an incompressible fluid, and the Navier–Stokes assumption is seen as leading to a simple diffusion of momentum. "It may seem a little strange that viscosity, which is a diffusion of momentum, can also diffuse energy and even Reynolds stresses. . . . A viscous stress acts both to convert mechanical energy into heat and to accelerate neighboring fluid, and this acceleration is an energy transfer. . . ." (Townsend 1956).
See Navier–Stokes equations.

Townsend, A. A. 1956. The Structure of Turbulent Shear Flow. Cambridge University Press, . p. 30.


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