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Ice Accretion Formations on a NACA 0012 Swept Wing Tip in Natural Icing Conditions

机译:自然结冰条件下,NACA 0012后掠式翼尖上的积冰形成

摘要

An experiment was conducted in the DeHavilland DHC-6 Twin Otter Icing Research Aircraft at NASA Glenn Research Center to study the formation of ice accretions on swept wings in natural icing conditions. The experiment was designed to obtain ice accretion data to help determine if the mechanisms of ice accretion formation observed in the Icing Research Tunnel are present in natural icing conditions. The experiment in the Twin Otter was conducted using a NACA 0012 swept wing tip. The model enabled data acquisition at 0 deg, 15 deg, 25 deg, 30 deg, and 45 deg sweep angles. Casting data, ice shape tracings, and close-up photographic data were obtained. The results showed that the mechanisms of ice accretion formation observed in-flight agree well with the ones observed in the Icing Research Tunnel. Observations on the end cap of the airfoil showed the same strong effect of the local sweep angle on the formation of scallops as observed in the tunnel.
机译:在NASA格伦研究中心的DeHavilland DHC-6双水獭结冰研究飞机上进行了一项实验,研究在自然结冰条件下扫掠机翼上积冰的形成。该实验旨在获取积冰数据,以帮助确定在自然结冰条件下是否存在在结冰研究隧道中观察到的积冰形成机制。在双水獭中的实验是使用NACA 0012后掠式翼尖进行的。该模型能够以0度,15度,25度,30度和45度扫掠角进行数据采集。获得了铸件数据,冰形描迹和特写摄影数据。结果表明,在飞行中观察到的积冰形成机理与在结冰研究隧道中观察到的机理相吻合。对翼型端盖的观察表明,与在隧道中观察到的一样,局部后掠角对扇贝形成的影响相同。

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