Let and use for the source's velocity gradient convention. Seek the homogeneous stationary stress reached under steady simple shear flow. The material derivative of that stress tensor vanishes. In the plane,
The , and components of the constitutive equation give, respectively,
Thus, putting and using the shear stress calculated below,
The out-of-plane shear components vanish on the homogeneous branch. The two normal-stress differences are
The ratio is defined at nonzero shear when ; at both differences vanish, and the displayed constant is their limiting ratio. An arbitrary isotropic pressure in the total Cauchy stress tensor cancels from both differences; it is not an arbitrary addition to the constitutively defined extra stress itself.

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