Experiments were conducted on the behaviour of the bubble plume in a step-stratification. The plume structures were divided into two patterns, depending on the plume number,
PΔ, the ratio of the stratification intensity to the bubbling rate. With
PΔ less than 10, the liquid plume breaks through up to the water surface, whereas with
PΔ higher than 10, a swell of the lower layer fluid forms on the interface. In addition, the height of the swell was described as a function of
PΔ. The water arriving at the free surface spreads radially along the free surface, and plunges into the water body. The spreading rate was expressed not only by
PΔ, but also by the ratio of the upper layer depth to the total one. Irrespective of the patterns, most of water rising into the upper layer, entrains the upper layer water, and falls down on to the density gap to form an intermediate layer there. The density distribution of the intermediate layer as well as the entrainment rate was measured. Then, using the entrainment rate and the volume flux of the plume, the evolution of the density profile was analyzed.
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