Paper 4, Section II, B

Fluid Dynamics II | Part II, 2011

A viscous fluid flows along a slowly varying thin channel between no-slip surfaces at y=0y=0 and y=h(x,t)y=h(x, t) under the action of a pressure gradient dp/dxd p / d x. After explaining the approximations and assumptions of lubrication theory, including a comment on the reduced Reynolds number, derive the expression for the volume flux

q=0hudy=h312μdpdxq=\int_{0}^{h} u d y=-\frac{h^{3}}{12 \mu} \frac{d p}{d x}

as well as the equation

ht+qx=0\frac{\partial h}{\partial t}+\frac{\partial q}{\partial x}=0

In peristaltic pumping, the surface h(x,t)h(x, t) has a periodic form in space which propagates at a constant speed cc, i.e. h(xct)h(x-c t), and no net pressure gradient is applied, i.e. the pressure gradient averaged over a period vanishes. Show that the average flux along the channel is given by

q=c(hh2h3)\langle q\rangle=c\left(\langle h\rangle-\frac{\left\langle h^{-2}\right\rangle}{\left\langle h^{-3}\right\rangle}\right)

where \langle\cdot\rangle denotes an average over one period.

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