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== General form ==
== General form ==
Reynolds' transport theorem, derived in <ref name=LGLp23>[[L. Gary Leal|L. G. Leal]], 2007, p. 23. </ref> <ref name=OR14>[[Osborne Reynolds|O. Reynolds]], 1903, Vol. 3, p. 14</ref>, is:
Reynolds' transport theorem, derived in <ref name=LGLp23>[[L. Gary Leal|L. G. Leal]], 2007, p. 23. </ref> <ref name=OR14>[[Osborne Reynolds|O. Reynolds]], 1903, Vol. 3, p. 14</ref>, <ref name=MTp23>[[Jerrold E. Marsden and Anthony Tromba|J. E. Marsden and A. Tromba]], 5th ed. 2003 </ref>is:
:<math>
:<math>
\cfrac{\mathrm{d}}{\mathrm{d}t}\int_{\Omega(t)} \mathbf{f}~\text{dV} =
\cfrac{\mathrm{d}}{\mathrm{d}t}\int_{\Omega(t)} \mathbf{f}~\text{dV} =

Revision as of 19:49, 20 November 2012

Reynolds' transport theorem (also known as the Leibniz-Reynolds' transport theorem), or in short Reynolds theorem, is a three-dimensional generalization of the Leibniz integral rule which is also known as differentiation under the integral sign. The theorem is named after Osborne Reynolds (1842–1912). It is used to recast derivatives of integrated quantities and is useful in formulating the basic equations of continuum mechanics.

Consider integrating over the time-dependent region that has boundary , then taking the derivative with respect to time:

If we wish to move the derivative under the integral sign there are two issues: the time dependence of , and the introduction of and removal of space from due to its dynamic boundary. Reynolds' transport theorem provides the necessary framework.

General form

Reynolds' transport theorem, derived in [1] [2], [3]is:

in which is the outward-pointing unit-normal, is a point in the region and is the variable of integration, and are volume and surface elements at , and is the velocity of the area element – so not necessarily the flow velocity.[4] The function may be vector or scalar valued. Note that the integral on the left hand side is a function solely of time, and so the total derivative has been used.

Form for a material element

In continuum mechanics this theorem is often used for material elements, which are parcels of fluids or solids which no material enters or leaves. If is a material element then there is a velocity function and the boundary elements obey

This condition may be substituted to obtain [5]

Erroneous sources

This theorem is widely quoted, incorrectly, as being the form specific to material volumes. See the planetmath external link below for an example. Clearly, if the material volume form is applied to regions other than material volumes, errors will ensue.

A special case

If we take to be constant with respect to time, then and the identity reduces to

as expected. This simplification is not possible if an incorrect form of the Reynolds transport theorem is used.

Interpretation and reduction to one dimension

The theorem is the higher dimensional extension of Differentiation under the integral sign and should reduce to that expression in some cases. Suppose is independent of & , and that is a unit square in the plane and has limits and . Then Reynolds transport theorem reduces to

which is the expression given on Differentiation under the integral sign, except that there the variables x and t have been swapped.

See also

Notes

  1. ^ L. G. Leal, 2007, p. 23.
  2. ^ O. Reynolds, 1903, Vol. 3, p. 14
  3. ^ J. E. Marsden and A. Tromba, 5th ed. 2003
  4. ^ Only for a material element there is
  5. ^ T. Belytschko, W. K. Liu, and B. Moran, 2000, Nonlinear Finite Elements for Continua and Structures, John Wiley and Sons, Ltd., New York.
  6. ^ Gurtin M. E., 1981, An Introduction to Continuum Mechanics. Academic Press, New York, p. 77.

References

L. G. Leal, 2007, Advanced transport phenomena: fluid mechanics and convective transport processes, Cambridge University Press, p. 912.

O. Reynolds, 1903, Papers on Mechanical and Physical Subjects, Vol. 3, The Sub-Mechanics of the Universe, Cambridge University Press, Cambridge.

  • Osborne Reynolds, Collected Papers on Mechanical and Physical Subjects, in three volumes, published circa 1903, now fully and freely available in digital format:
Volume 1
Volume 2
Volume 3