Effect of downstream control on stability and mixing of a vertical plane buoyant jet in confined depth

The effect of downstream control on the mixing of a plane turbulent heated jet discharging vertically into confined depth is studied using the buoyanc y extended k-epsilon model. The steady two-dimensional turbulent flow, temp erature and turbulence fields are computed using the finite volume method o n a high resolution grid. In the absence of a specific downstream control, the numerical predictions demonstrate three generic flow patterns for diffe rent jet discharges and environmental parameters: i) a flow with circulatio n cells of alternate rotation for non-buoyant discharge; ii) a stable buoya nt discharge with the mixed fluid leaving the vertical jet region in a surf ace warm water layer; and iii) an unstable buoyant discharge with flow reci rculation and re-entrainment of heated water. A stratified counterflow regi on always appears in the far-field for both stable and unstable buoyant dis charges. The near field interaction and hence discharge stability is govern ed by only two dimensionless parameters - the discharge densimetric Froude number F-o and the depth to jet width ratio H/B. The computed velocity and temperature fields agree well with the laboratory flow- visualization and t emperature measurements of Jirka & Harleman (1979). Numerical prediction of stability categories is in excellent agreement with experiments. For a giv en discharge and depth, it is found that the jet stability can be predicted regardless of downstream control, provided that the channel length exceeds about 6H. The effect of a strong downstream control close to the discharge primarily results in a flooded internal jump and the lowering of the inter face level in the stratified counterflow region. Consistent with the detail ed measurements of Andreopoulos, Praturi and Rodi (1986), the predictions s how a clear reduction of the bulk dilution, although the effect of downstre am control on the jet discharge stability is insignificant.