In this report the evolution of layering and the mechanism of degradation of layers formed from a stably stratified solution between the heated and cooled vertical parallel plates are precisely discussed. The relationship between
Ra,
f which expresses the dimensionless parameter of temperature fluctuation in the layer and
Ra,
w which is related to the intensity of the natural convection flow induced by the heated and cooled walls is obtained. When
Ra,
w is less than 15000,
Ra,
f increases with the increase of
Ra,
w and the flow is laminar. When
Ra,
w is between 15000 and 25000,
Ra,
f increases rapidly with the increase of
Ra,
w and the transition to turbulence occurs. The analysis shows that the temperature fluctuation in the layer is attenuated due to the transfer of heat across the interfaces contacting with upper and lower layers and the horizontal convection flow disappears when the critical value of
Ra,
w is 16800.
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