For oscillations at frequency ω, a viscous penetration depth δv can be defined by
δv=(ρω2η)1/2,(10.76)
analogously to the thermal penetration depth
δ=(ρcpω2κ)1/2(10.77)
defined in this chapter. Show that
(δδv)2=σp,(10.78)
where σp is the Prandtl number (see eqn 10.59).