Algebra of Communicating Processes

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In continuum mechanics, including fluid dynamics, an upper-convected time derivative or Oldroyd derivative, named after James G. Oldroyd, is the rate of change of some tensor property of a small parcel of fluid that is written in the coordinate system rotating and stretching with the fluid.

The operator is specified by the following formula:

𝐀▽=DDtπ€βˆ’(βˆ‡π―)Tβ‹…π€βˆ’π€β‹…(βˆ‡π―)

where:

The formula can be rewritten as:

Aβ–½i,j=βˆ‚Ai,jβˆ‚t+vkβˆ‚Ai,jβˆ‚xkβˆ’βˆ‚viβˆ‚xkAk,jβˆ’βˆ‚vjβˆ‚xkAi,k

By definition the upper-convected time derivative of the Finger tensor is always zero.

The upper-convected derivative is widely use in polymer rheology for the description of behavior of a viscoelastic fluid under large deformations.

Examples for the symmetric tensor A

For the case of simple shear:

βˆ‡π―=(000Ξ³Λ™00000)

Thus,

𝐀▽=DDtπ€βˆ’Ξ³Λ™(2A12A22A23A2200A2300)

Uniaxial extension of uncompressible fluid

In this case a material is stretched in the direction X and compresses in the direction s Y and Z, so to keep volume constant. The gradients of velocity are:

βˆ‡π―=(Ο΅Λ™000βˆ’Ο΅Λ™2000βˆ’Ο΅Λ™2)

Thus,

𝐀▽=DDtπ€βˆ’Ο΅Λ™2(4A11A12A13A12βˆ’2A22βˆ’2A23A13βˆ’2A23βˆ’2A33)

See also

References

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