Let , , and , so the single-bead mobility is . Assume an incompressible solvent, constant , negligible bead inertia, and a symmetric positive-definite . The last requirement makes the resistance invertible and Brownian diffusion physically admissible. At a given position and time, depends on the moment but not on the individual configuration .
Use the source's gradient convention , and write for the component-first gradient. Then . The spring forces on the two beads are and . Their overdamped probability currents are
Here the Brownian term written as is a force weighted by probability density. Its corresponding conditional osmotic force is ; treating the given term as an unweighted deterministic force per bead would not produce the stated Fokker–Planck equation.
With midpoint , the derivatives are and . Subtracting the bead currents gives the configuration current
The midpoint current is after neglecting the specified spatial Brownian diffusion. Configuration probability conservation therefore gives
Since has components , this agrees with the source's . The factor two in both spring relaxation and configuration diffusivity comes from relative motion of both beads.
The second moment is the unnormalized conformation tensor. Now multiply by and integrate over configuration space. Assume sufficiently decaying tails so every boundary term at infinite separation vanishes. The affine current gives ; spring drift gives ; two integrations by parts of diffusion give . Hence
Because , is a polynomial in and commutes with it. Thus
This is the Hookean dumbbell conformation equation with anisotropic mobility, an exact second-moment closure within the stated model; no Gaussian approximation to was needed.
The upper-convected derivative of the identity is . Applying it to the polymer stress therefore gives
Consequently the coefficients and the closed stress equation are
where in the printed convention. Here is a polymer relaxation time, unrelated to the inverse-length parameter of question c; is the polymer viscosity scale. The coefficient has inverse-stress units. In the dimensional mobility parameter in the Giesekus model, the dimensionless factor is , not the dimensional printed in this problem.
The upper-convected rate removes the affine stretching and rotation of material connectors. If , then a tensor transported purely as has . Under a time-dependent rigid rotation , the rate transforms as : this is material frame indifference, not an ordinary componentwise time derivative. The resulting equation is the Giesekus model in these dimensional conventions.
The isotropic subtraction is fixed by zero polymer extra stress at thermal equilibrium. With no flow and positive mobility, the stationary distribution is
so . The constitutive equation correspondingly has a zero-stress quiescent state and a Newtonian low-rate limit . Without subtracting exactly , the spring contribution would retain an equilibrium isotropic stress and the equation would acquire corresponding reference terms. Because mobility itself depends on , that reference cannot simply be shifted while retaining the same model. The separate fluid pressure enforcing incompressibility is not included in this polymer extra stress.