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An experimental and computational investigation of slender wings undergoing wing rock.

机译:经历机翼岩石的细长机翼的实验和计算研究。

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The problem of self-induced roll oscillations of slender delta wings has been studied in order to identify physical mechanisms responsible for the limit cycle oscillations. The investigation is a combination of both experimental and computational methodologies. The experimental and computational investigations focussed on the wing rock characteristics of a slender flat plate delta wing with 80{dollar}spcirc{dollar} leading edge sweep.; Two unique experimental apparatus have been developed for the investigation. A free to roll system was developed using an air bearing spindle which allows the isolation of applied torques due to the flowfield. An unsteady pressure acquisition system was also developed in order to measure the unsteady surface pressure distributions acting on the wing during wing rock time histories. The system consists of a motion control system which accurately matches the time dependent boundary conditions of wing rock, and is synchronized with a pressure acquisition system.; The computational model is a discrete vortex potential flow method. The time dependent positions and strengths of the leading edge vortices are solved by coupling the flowfield equations to the rigid body equation of motion in roll for the wing. The computational model has captured all of the qualitative characteristics of the wing motion and flowfield behavior observed in experiment with the exception of the secondary vortices which are not modelled.; Based on the results of the experimental and computational investigations a theory has been developed for the cause of wing rock of slender wings. The theory is broad enough to account for variations in sweep angle and angle of attack. Wing rock is initiated by some initial perturbation or wing imperfection. The motion builds in time due to an instability caused by a time lag in the position of the vortices normal to the wing surface. A steady state is reached when damping contributions from the top and bottom surfaces are in equilibrium with the instability. Damping is provided by conventional roll damping on the bottom surface of the wing, and by the unsteady behavior of vortex strength on the top surface.
机译:为了确定引起极限循环振荡的物理机制,已经研究了细长三角翼的自感应侧倾振荡问题。该研究是实验和计算方法学的结合。实验和计算研究集中在细长的平板三角翼上,其前缘掠过角为80 {spcirc {dollar}。已经开发出两种独特的实验仪器进行研究。使用空气轴承主轴开发了一种自由滚动系统,该主轴可以隔离由于流场而产生的扭矩。为了测量机翼岩石时间历史过程中作用于机翼的非稳态表面压力分布,还开发了非稳态压力采集系统。该系统由运动控制系统组成,该系统精确地匹配了随时间变化的机翼岩石边界条件,并与压力采集系统同步。该计算模型是离散涡旋势流方法。通过将流场方程与机翼侧倾运动中的刚体运动方程耦合来解决前缘涡旋的时间相关位置和强度。该计算模型捕获了实验中观察到的机翼运动和流场特性的所有定性特征,除了未建模的次级涡流。根据实验和计算研究的结果,为细长机翼的机翼岩石的成因发展了一个理论。该理论足够广泛,可以解释扫掠角和迎角的变化。机翼岩石是由一些初始扰动或机翼缺陷引起的。由于在垂直于机翼表面的旋涡位置中存在时间滞后而导致的不稳定性,从而使运动及时建立。当顶面和底面的阻尼作用与不稳定性达到平衡时,将达到稳态。通过机翼底面上的常规侧倾阻尼以及顶面上涡流强度的不稳定行为,可以提供阻尼。

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