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摘要

RICHTER, SULLIVAN,国家大气研究中心—在位于海气界面上方的大气表层,大风可以将大量的海沫喷射到上方的湍流中。紊流表层的这种分散相是否能改变从空气到海洋表面的动量转移,这个问题仍然没有解决。因此,这项研究的目的是确定和解释在紊流、粒子流中壁法向动量传递的变化。这是通过使用离散相的拉格朗日点粒子表示的直接数值模拟(DNS)完成的。选择湍流库埃特流,是因为它表现出与大气表层相似的某些特征,研究了不同浓度和大小的球形非相互作用颗粒。一般来说,分散相的加入破坏了导致湍流、载流子相动量转移的运动,同时通过额外的分散相应力补偿了这种动量转移的损失。本文将介绍紊流壁-法向动量输运中这些变化的机理和解释。
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The Meeting
Hilbert University — There are two major theories of probability, one due to von Mises and the other due to Kolmogorov. The first requires the existence of a collective before probabilities can be defined. Its motivation is physical. The second postulates a probability space which is purely mathematical. It makes probability a branch of mathematics. We show that von Mises’ theory is more appropriate to application in quantum theory. Kolomogorov’s theory can lead to paradoxical results.
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