词条 | Upper-convected time derivative |
释义 |
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: where:
The formula can be rewritten as: By definition the upper-convected time derivative of the Finger tensor is always zero. It can be shown that the upper-convected time derivative of a spacelike vector field is just its Lie derivative by the velocity field of the continuum.[1] 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 ASimple shearFor the case of simple shear: Thus, Uniaxial extension of incompressible fluidIn this case a material is stretched in the direction X and compresses in the directions Y and Z, so to keep volume constant. The gradients of velocity are: Thus, See also
References
1. ^{{cite journal|last1=Matolcsi|first1=Tamás|last2=Ván|first2=Péter|title=On the Objectivity of Time Derivatives|date=2008|doi=10.1478/C1S0801015}} 3 : Multivariable calculus|Fluid dynamics|Non-Newtonian fluids |
随便看 |
|
开放百科全书收录14589846条英语、德语、日语等多语种百科知识,基本涵盖了大多数领域的百科知识,是一部内容自由、开放的电子版国际百科全书。