磁共振测速技术在崎岖地形中的三维速度场测量

D. Chung
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引用次数: 0

摘要

磁共振成像技术被用于收集新墨西哥州一个峡谷的三维速度数据,并与峡谷内气体释放的模拟进行比较。第一个峡谷模型面积为1850m × 1030m,比例为1:5250;第二个模型面积为290m × 160m,比例为1:825。在两种模型中,雷诺数为36000的完全湍流通过峡谷几何形状。磁共振测速仪(MRV)测量了超过1300万个数据点来表示流速。1:5250比例尺模型的MRV实验有助于确定下一组更高分辨率模型测量中包含的关键地形特征。MRV不仅是一种分析方法,也是一种设计方法。对数据的分析导致了1:825比例尺的新设计,该比例尺对气体释放点周围的地形具有更高的分辨率。1:825比例模型的初步扫描显示,与1:5250比例模型相比,释放点周围的流动更加动态。在1:825比例模型中可以观察到反向旋转的涡旋和环流。该数据集将用于与桑迪亚国家实验室在复杂地形中紊流的模拟进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Three-Dimensional Velocity Field Measurements in Rugged Terrain Using Magnetic Resonance Velocimetry
Magnetic resonance imaging techniques were used to collect three-dimensional velocity data measurements of scaled models of a canyon in New Mexico to compare to simulations where a gas was released inside the canyon. The first canyon model covers an area of 1850m × 1030m with a scale of 1:5250 while the second model covers an area of 290m × 160m with a scale of 1:825. A fully turbulent flow with a Reynolds number of 36,000 using the channel hydraulic diameter passes through the canyon geometry for both models. With Magnetic Resonance Velocimetry (MRV), more than 13 million data points were measured to represent flow velocity. The MRV experiment with the 1:5250 scale model helped to identify key terrain features to be included in the next set of measurements of a higher resolution model. MRV not only served as a method of analysis but also as a method for design. The analysis of the data resulted in a new design of a 1:825 scale, which had a higher resolution of the terrain surrounding the gas release point. The preliminary scans from the 1:825 scale model showed a much more dynamic flow around the release point than observed in the 1:5250 scale model. Counter-rotating vortices and circulation can be observed in the 1:825 scale model. This data set will be used to compare to Sandia National Laboratories’ simulations of turbulent flows in a complex terrain.
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