论文部分内容阅读
A dual-time method is introduced to calculate the unsteady flow in a certain vibrating fiat cascade.An implicit lower-upper symmetric-gauss-seidel scheme(LU-SGS) is applied for time stepping in pseudo time domains,and the convection items are discretized with the spatial three-order weighted non-oscillatory and non-free-parameter dissipation difference (WNND) scheme.The turbulence model adopts q-ωlow-Reynolds-number model.The frequency spectrums of lift coefficients and the unsteady pressure-difference coefficients at different spanwise heights as well as the entropy contours at blade tips on different vibrating instants,are obtained.By the analysis of frequency spectrums of lift coefficients at three spanwise heights,it is considered that there exist obvious non-linear perturbations in the flow induced by the vibrating,and the perturbation frequencies are higher than the basic frequency.The entropy contours at blade tips at different times display an intensively unsteady attribute of the flow under large amplitudes.
A dual-time method is introduced to calculate the unsteady flow in a certain vibrating fiat cascade. An implicit lower-upper symmetric-gauss-seidel scheme (LU-SGS) is applied for time stepping in pseudo time domains, and the convection items are discretized with the spatial three-order weighted non-oscillatory and non-free-parameter dissipation difference (WNND) scheme.The turbulence model adopts q-ωlow-Reynolds-number model.The frequency spectrums of lift coefficients and the unsteady pressure-difference coefficients at different spanwise heights as well as the entropy contours at blade tips on different vibrating instants, are obtained. By the analysis of frequency spectrums of lift coefficients at three spanwise heights, it is considered that there exist obvious non-linear perturbations in the flow induced by the vibrating, and the perturbation frequencies are higher than the basic frequency. entropy contours at blade tips at different times display an intensively unsteady attribute of the flow under large amplitudes.