Heat-transport measurements in a normal-fluid ³-⁴He mixture contained in a porous medium and heated from below show a bifurcation to steady or oscillatory flow, depending on the mean temperature. With increasing Rayleigh number R the oscillatory state is entered via a forward Hopf bifurcation with frequency ωc>0. As the stationary bifurcation is approached by change of the mean temperature, ωc vanishes. With increasing R, the oscillatory state terminates with vanishing frequency and finite amplitude in a hysteretic bifurcation to a steady state. Those observations agree with recent theoretical predictions.
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Rehberg et al. (1985) studied this question.
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