A method for predicting the velocity profile in a one‐dimensional, slow moving, laminar fluid in which yield stress varies with depth is presented in this paper. The governing equations are solved for two types of yield stress gradients [ and ]. The depth of the flowing layer and velocity profile are given as algebraic equations in these cases. A yield stress gradient can exist whenever high concentrations of fine‐grained solids are settling and compacting (e.g., dredged material containment area, high‐rate settler).
Topics
Mechanical stress
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© 1980 The Society of Rheology.
1980
The Society of Rheology
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