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首页> 外文期刊>Journal of Volcanology and Geothermal Research2012V243-244NOCT,15 >The terminal velocity of volcanic particles with shape obtained from 3D X-ray microtomography
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The terminal velocity of volcanic particles with shape obtained from 3D X-ray microtomography

机译:通过3D X射线显微断层摄影术获得的具有形状的火山颗粒的最终速度

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摘要

New experiments of falling volcanic particles were performed in order to define terminal velocity models applicable in a wide range of Reynolds number Re. Experiments were carried out with fluids of various viscosities and with particles that cover a wide range of size, density and shape. Particle shape, which strongly influences fluid drag, was measured in 3D by High-resolution X-ray microtomography, by which sphericity Phi(3D) and fractal dimension D-3D were obtained. They are easier to measure and less operator dependent than the 2D shape parameters used in previous papers. Drag laws that make use of the new 3D parameters were obtained by fitting particle data to the experiments, and single-equation terminal velocity models were derived. They work well both at high and low Re (3 x 10(-2)
机译:为了定义适用于广泛雷诺数Re的终极速度模型,进行了下落的火山颗粒的新实验。实验是使用各种粘度的流体以及覆盖各种尺寸,密度和形状的颗粒进行的。通过高分辨率X射线显微照相术在3D中测量了强烈影响流体阻力的颗粒形状,从而获得了球形度Phi(3D)和分形维数D-3D。与以前的论文中使用的2D形状参数相比,它们更易于测量且对操作者的依赖性较小。通过将粒子数据拟合到实验中,获得了使用新3D参数的阻力定律,并推导了单方程终端速度模型。它们在高和低Re(3 x 10(-2)

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