Influence of the Coriolis Force on the Flow in a Low Pressure Turbine Cascade T106
The paper presents numerical investigations of a model setup conceived to investigate the influence of the Coriolis force on the secondary flow in a low pressure turbine cascade. It addresses the question in which sense and by how much results in a linear cascade may differ from the situation in a rotating cascade. For this purpose highly resolved Direct Numerical Simulations of the flow within a T106A passage close to the endwall were conducted for two cases with and without rotation and hence with and without Coriolis force at a Reynolds number of 20,000. Comparing non-rotating and rotating turbine passage, several effects are detected: First, the Coriolis force causes transition of the horseshoe vortices, so that the region between the blades becomes much more turbulent and an explanation for the destabilization is provided. Second, the strong radial flow caused by the Coriolis force suppresses the laminar separation of the boundary flow at the suction side. Third, in the case with rotation, the large-scale secondary motion creates higher stagnation pressure loss than in the reference case and is responsible for a complete redistribution of the flow field in the passage. An additional test case with opposite rotation was computed for completeness.