A plain material derivative of the conformation tensor is not an objective time derivative: an observer undergoing a time-dependent rigid rotation would infer a different constitutive response, and even rigid-body rotation could appear to change polymer deformation. The upper-convected derivative subtracts deformation and rotation carried by the velocity gradient and is frame indifferent.
The Oldroyd-B model is often inadequate because its Hookean dumbbells are infinitely extensible. It predicts constant shear viscosity rather than shear thinning, zero second normal-stress difference, and an unbounded extensional viscosity at a finite extension rate. Real polymer chains have finite extensibility and commonly exhibit shear thinning, bounded extensional stress, multiple relaxation times, and nonlinear solvent or concentration effects.
Let . For simple shear, the steady conformation equation is
Its nonzero components are
Since ,
Thus the FENE-P model has
The trace is
Substituting it into gives
For , . For , . The effective shear viscosity is therefore
The FENE-P curve decreases from toward the solvent plateau , displaying shear thinning. Oldroyd-B has and remains at the constant value .
For uniaxial extension,
The diagonal steady conformation tensor is
where physical solutions require . The extensional viscosity is
The implicit closure is
As , , , and
The Trouton ratio is therefore three. This is also the small-rate Oldroyd-B result because finite extensibility is irrelevant while polymer deformation remains small.
For FENE-P at , write . The trace constraint approaches the finite maximum , so and to leading order. Hence
up to corrections that vanish as . Its extensional viscosity rises from the Newtonian plateau and saturates at a finite-extensibility plateau.
For Oldroyd-B, and
It diverges as and has no physical steady homogeneous branch beyond that point. This extensional catastrophe is removed by finite chain extensibility.

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