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作 者:李熙[1,2]
机构地区:[1]河海大学海岸灾害及防护教育部重点实验室,南京210098 [2]河海大学交通与海洋工程学院,南京210098
出 处:《水动力学研究与进展(A辑)》2008年第2期226-229,共4页Chinese Journal of Hydrodynamics
摘 要:在实验室中翻转两层或三层的非牛顿液体,初始分层是稳定的。翻转水箱具有相对较小的厚度,翻转后产生的湍流是虚三维的(Pesdo-3D),瑞利泰勒不稳定性起动了湍流混合过程及前锋的行进。时间的典型测量是从最初稳定的时间开始后两妙,而翻转过程的是大约1秒,本文采用相对密度的均方根扰动分析了两组数据,关于反转涡系级联(cascade)的有限时间爆破的猜想首次在实验通过定义两个特征时间被证实:均方根扰动(RMS)的第一个峰值时间,T1;湍流前锋触底时间,Tf,得出结论,当引入标量时间ts1时,T1/ts1逼近Tf。Abstract: A laboratory study of mixing in non-Newton fluids of blood was conducted by overturning a tank of initially stable stratified fluids of two or three layers. The tank was of comparably small thickness and the turbulence subsequent to the instabilities was pseudo-3D. The Rayleigh-Taylor instabilities initiated the turbulent mixing and front advancement of turbulence. Typically the measurement was started 2 seconds calculated from initial stable condition and the overturning process is about 1 second, two sets of data were analyzed by excess density RMS (root mean square) fluctuation, conjecture of finite time blow-up of overturned eddies cascade was confirmed first in laboratory by relating two characteristic times: the first peak time of RMS, T1; front reaching lower boundary time, Tf. It is concludedT1 / ts1 approximates Tf by introducing a scalar of time scale ta1.
分 类 号:TV131[水利工程—水力学及河流动力学]
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