At the final state of the slump test for yield stress, an axisymmetric deposit of height is just able to support itself. Hydrostatic pressure gives radial pressure gradient , while lubrication theory makes the magnitude of the basal shear stress
The marginally yielded final profile therefore satisfies
Integration gives
Using mass conservation, the known volume is
Solving for the yield stress produces the estimate
Thus one measures the final radius and inserts it with and . The estimate assumes a thin deposit, negligible surface tension, complete initial yielding, and a spatially uniform yield stress.
Dry sand is a granular material governed primarily by frictional stability. Its final free surface reaches the angle of repose , so the deposit is approximately a cone,
This constant-slope profile differs from the square-root edge of the yield-stress-fluid model.

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