雷诺兹数缩放和能量光谱在地质对流的对流
Matteo Madonia1, Andrés J Aguirre Guzmán1, Herman J H Clercx1
1Fluids and Flows group, Department of Applied Physics and J. M. Burgers Centre for Fluid Dynamics, Eindhoven University of Technology, P.O. Box 513, 5600 MB Eindhoven, The Netherlands.
概括
研究人员研究了旋转的雷利-贝纳德对流,观察流动力学和速度缩放. 结果表明,随着Ekman数的减少,乱的散装流状态正在接近.
科学领域:
- 流体动力学 流体动力学
- 地质物理学 地质物理学
- 流是什么?流是什么?流是什么?
背景情况:
- 旋转的雷利-贝纳德对流是地球物理流的一个关键模型.
- 了解地层对流需要分析力平衡和流动模式.
研究的目的:
- 为了研究在地质系内旋转雷利-贝纳德对流的流量测量.
- 为了比较速度波动缩放与理论力量平衡 (VAC和CIA).
- 探索向无扩散流状态的过渡.
主要方法:
- 立体粒子图像速度计 (PIV) 用于测量3D速度组件.
- 实验是在一个圆柱形的对流容器中进行的,在一个固定的Ekman数 (Ek) 上,具有不同的雷利数 (Ra).
- 分析了流量数据的速度缩放,动能光谱和力量平衡影响.
主要成果:
- 粘性-阿基米德-科里奥利斯 (VAC) 和科里奥利斯-惯性-阿基米德 (CIA) 两种力平衡都显示出与速度缩放的良好一致.
- 随着Ekman数的减少,观察到向无扩散速度缩放的趋同.
- 动能光谱显示了四极旋结构,以及在更高的Ra时出现-5/3缩放范围的发展,这是3D流的特征.
结论:
- 这项研究提供了证据,证明了在旋转对流中实现完全发达,无扩散的乱散流状态的方法.
- 观察到的流体组织和光谱缩放表明了与地球物理现象相关的复杂动态.
- 进一步的研究是有必要的,以充分阐明这个政权的动荡动态.
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