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Stereoscopic measurements of particle dispersion in microgravity turbulent flow.

机译:立体测量微重力湍流中的颗粒分散。

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The presence of particles in turbulent flows adds complexity to an already difficult subject. The work described in this research dissertation was intended to characterize the effects of inertia, isolated from gravity, on the dispersion of solid particles in a turbulent air flow. The experiment consisted of releasing particles of various sizes in an enclosed box of fan-generated, homogenous, isotropic, and stationary turbulent airflow and examining the particle behavior in a microgravity environment. The turbulence box was characterized in ground-based experiments using laser Doppler velocimetry techniques. Microgravity was established by free-floating the experiment apparatus during the parabolic trajectory of NASA's KC-135 reduced gravity aircraft. The microgravity generally lasted about 20 seconds, with about fifty parabolas per flight and one flight per day over a testing period of four days.; To cover a broad range of flow regimes of interest, particles with Stokes numbers (St) of 1 to 300 were released in the turbulence box. The three-dimensional measurements of particle motion were made using a three-camera stereo imaging system with a particle-tracking algorithm. Digital photogrammetric techniques were used to determine the particle locations in three-dimensional space from the calibrated camera images. The epipolar geometry constraint was used to identify matching particles from the three different views and a direct spatial intersection scheme determined the coordinates of particles in three-dimensional space. Using velocity and acceleration constraints, particles in a sequence of frames were matched resulting in particle tracks and dispersion measurements.; The goal was to compare the dispersion of different Stokes number particles in zero gravity and decouple the effects of inertia and gravity on the dispersion. Results show that higher inertia particles disperse less in zero gravity, in agreement with current models. Particles with St ≈ 200–300 dispersed about 110 of the dispersion measured in St ≈ 1 particles. Similarly, fluid points were shown to disperse 25 times as much as St ≈ 1 particles. Particles with more inertia also have particle velocity autocorrelations that decay more slowly. Comparisons are made with previous experimental work and indicate 40% less dispersion with gravity for St ≈ 1 particles and a slower decorrelation rate.
机译:湍流中颗粒的存在增加了本来就很困难的问题的复杂性。本研究论文中描述的工作旨在表征与重力隔离的惯性对湍流中固体颗粒分散的影响。该实验包括在密闭的风扇产生的,均质的,各向同性的和固定的湍流气流的盒子中释放各种尺寸的颗粒,并检查微重力环境中的颗粒行为。在基于地面的实验中,使用激光多普勒测速技术对湍流箱进行了表征。通过在NASA的KC-135重力飞行器的抛物线轨迹中自由浮动实验装置来建立微重力。微重力通常持续约20秒,在四天的测试期内,每次飞行约有50个抛物线,每天飞行1次。为了涵盖各种感兴趣的流动方式,斯托克斯数( St )为1到300的粒子在湍流箱中被释放。使用具有粒子跟踪算法的三相机立体成像系统对粒子运动进行了三维测量。使用数字摄影测量技术从校准的相机图像确定三维空间中的粒子位置。对极几何约束用于从三个不同的视图识别匹配的粒子,并且直接的空间相交方案确定了三维空间中粒子的坐标。使用速度和加速度约束,对一系列帧中的粒子进行匹配,从而进行粒子轨迹和色散测量。目的是比较零重力下不同斯托克斯数粒子的色散,并消除惯性和重力对色散的影响。结果表明,与当前模型一致,较高惯性的粒子在零重力下的分散较少。 St ≈的粒子200–300左右分散度的 1 10 左右圣≈ 1个颗粒。同样,流体点的分散度是 St ≈的25倍。 1个颗粒。具有较大惯性的粒子也具有粒子速度自相关,其衰减速度较慢。与之前的实验工作进行了比较,结果表明 St ≈的重力分散度降低了40%。 1个粒子和较低的去相关速率。

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