The convective properties of a water layer near 4 °C have been examined by means of local velocity measurements. The non linear density profile of such a layer produces qualitatively different behaviour from that observed in « Boussinesq » fluids. In particular a hexagonal dissipative structure is observed corresponding to an abnormal bifurcation near the threshold ; at higher Rayleigh numbers, these hexagons transform into asymmetric two-dimensional rolls. The measured velocity field is in agreement with that expected from the breakdown in the symmetry properties of the water layer.
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Dubois et al. (1978) studied this question.
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