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Numerical Investigation of Laminar-Turbulent Transition in a Cone Boundary Layer at Mach 6

机译:6马赫锥边界层内层流-湍流过渡的数值研究

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摘要

Direct Numerical Simulations (DNS) are performed to investigate laminar-turbulent transition in a boundary layer on a sharp cone at Mach 6. The main objective of this dissertation research is to explore which nonlinear breakdown mechanisms may be dominant in a broad--band "natural" disturbance environment and then use this knowledge to perform controlled transition simulations to investigate these mechanisms in great detail. Towards this end, a "natural" transition scenario was modeled and investigated by generating wave packet disturbances. The evolution of a three-dimensional wave packet in a boundary layer has typically been used as an idealized model for "natural" transition to turbulence, since it represents the impulse response of the boundary layer and, thus, includes the interactions between all frequencies and wave numbers. These wave packet simulations provided strong evidence for a possible presence of fundamental and subharmonic resonance mechanisms in the nonlinear transition regime. However, the fundamental resonance was much stronger than the subharmonic. In addition to these two resonance mechanisms, the wave packet simulations also indicated the possible presence of oblique breakdown mechanism. To gain more insight into the nonlinear mechanisms, controlled transition simulations were performed of these mechanisms. Several small and medium scale simulations were performed to scan the parameter space for fundamental and subharmonic resonance. These simulations confirmed the findings of the wave packet simulations, namely that, fundamental resonance is much stronger compared to the subharmonic resonance. Subsequently a set of highly resolved fundamental and oblique breakdown simulations were performed. In these DNS, remarkable streamwise arranged "hot'' streaks were observed for both fundamental and oblique breakdown. The streaks were a consequence of the large amplitude steady longitudinal vortex modes in the nonlinear régime. These simulations demonstrated that both second--mode fundamental breakdown and oblique breakdown may indeed be viable paths to complete breakdown to turbulence in hypersonic boundary layers at Mach 6.
机译:进行了直接数值模拟(DNS),以研究6马赫数的尖锥上边界层中的层流湍流过渡。本论文研究的主要目的是探讨在宽带“自然”干扰环境,然后使用此知识执行受控的过渡模拟,以详细研究这些机制。为此,通过产生波包扰动对“自然”过渡情景进行了建模和研究。边界层中三维波包的演化通常被用作“自然”过渡到湍流的理想模型,因为它表示边界层的冲激响应,因此包括所有频率和频率之间的相互作用。波数。这些波包模拟为非线性过渡机制中可能存在基本和次谐波共振机制提供了有力的证据。但是,基本共振比次谐波要强得多。除了这两种共振机制外,波包模拟还表明可能存在倾斜破坏机制。为了更深入地了解非线性机制,对这些机制进行了受控过渡仿真。进行了几个中小型仿真,以扫描参数空间的基本和次谐波共振。这些模拟证实了波包模拟的发现,即与次谐波共振相比,基本共振要强得多。随后进行了一组高度解析的基本和倾斜击穿仿真。在这些DNS中,基本和倾斜击穿都观察到了明显的沿流方向排列的“热”条纹,这些条纹是非线性制度中大振幅稳定纵向涡模的结果,这些模拟表明,第二模式基本击穿倾斜击穿确实是在6马赫高超声速边界层中彻底击碎湍流的可行途径。

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    Sivasubramanian Jayahar;

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  • 年度 2012
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