A Taylor swimming sheet beneath a finite Brinkman layer is slower than in a Newtonian fluid unless the layer is thin, highly permeable, close to the sheet, or has a positive jump stress.
Figure 4(d) further illustrates the maximum achieved in the scaled swimming speed, Us, at small Brinkman constants, k, and δ H = 1
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A Taylor swimming sheet under a finite Brinkman layer
A Taylor swimming sheet beneath a finite Brinkman layer is slower than in a Newtonian fluid unless the layer is thin, highly permeable, close to the sheet, or has a positive jump stress.