Let be the rate-of-strain tensor. A Newtonian fluid has a linear isotropic constitutive law for its viscous stress tensor. To determine its form, diagonalize the symmetric tensor . Rotations by about its principal axes leave fixed, forcing its stress response to be diagonal as well. Linearity and symmetry under permutations of the axes force each diagonal entry to be , with the same constants for each axis. Rotating back gives . Since incompressibility means , adding the arbitrary isotropic pressure givesAt a material interface between ordinary viscous fluids without interfacial slip, velocity is continuous, and its normal component equals the interface's normal speed. Tangential traction is continuous when surface tension is constant. Normal traction has the curvature-dependent surface tension jump; in a convention defining signed curvature by the balance, . With no surface tension, the full traction is continuous. At rigid stationary walls the no-slip boundary condition imposes zero velocity.
Put and seek . The convective acceleration vanishes, and the Navier-Stokes equations reduce to , with . continuity of velocity and tangential traction at gives a common interface velocity and a common shear integration constant :Imposing givesThe velocity has no normal component, so the flat interface remains stationary, and its normal stresses match because pressure is common. These expressions give the two-layer plane Poiseuille flow with unequal viscosities.
The signed tangential stress component is . ThusWhen , these approach and , the usual symmetric plane Poiseuille flow stresses. When , they approach and . The upper fluid's velocity tends to zero, but its viscosity times velocity gradient has a finite limit. These are tensor components; traction on a chosen wall normal includes that normal's sign.
Integrating the velocity profiles over their respective half-channels gives volume flux per unit widthWith , the requested ratio isAt , both fluxes equal and the ratio is one. For , , and the ratio is asymptotic to , tending to zero. The lower fluid flows between the wall and an interface which becomes effectively stationary; the upper fluid carries vanishing flux despite finite limiting stress.
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