Under the plug-like extensional viscosity approximation, incompressibility gives . Symmetry about fixes . Remove the reference hydrostatic stress of the middle fluid, and write for its leading vertical normal stress. Vertical traction balance at the upper surface gives
The middle fluid's horizontal normal stress exceeds by : the horizontal strain is and the vertical strain is . Hence
At a slightly inclined upper interface, tangential traction continuity gives, to the order retained in the small-outer-viscosity extensional approximation,
The slope term is needed even though the interface is nearly horizontal: dropping it would miss the derivative of in the extensional resultant. Terms involving the outer deviatoric normal-stress difference times the slope are smaller in this approximation. Integrating horizontal force balance over the symmetric layer, or over its upper half, now gives
Substitution yields the extensional-flow equation
The full layer thickness is , so its conservation of mass is , or
This explains the factor in the extensional stress rather than the shear viscosity coefficient alone.
For a Fourier mode of wave number , set and . Neglect as stipulated. The Fourier traction map for a viscous half-space, with outer dynamic viscosity , gives . The two linear equations are
Eliminating proves the positive decay rate for relaxation of a symmetric viscous layer:
When , inner longitudinal extension dominates the viscous dissipation, and . When while the plug approximation remains valid, tangential motion of the semi-infinite outer fluids supplies the main resistance, and . The PDF's second inequality is ; the TeX converts it incorrectly to . At much larger outer viscosity the plug assumption fails, as the next calculation shows.