Viscoelastic Taylor–Couette instability in the Keplerian regime

IF 1.1 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
Y. Bai, T. Vieu, O. Crumeyrolle, I. Mutabazi
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引用次数: 3

Abstract

Instability modes of viscoelastic Taylor–Couette flow in the Keplerian regime are investigated using both linear stability analysis and experimental detection of critical states. A generalised Rayleigh criterion has been derived and it allows to separate the zone of potential purely elastic instability modes and the zone of stability. The analogy between the instability of viscoelastic Taylor–Couette flow in the Keplerian regime and the magnetorotational instability (MRI) of conducting magnetic fluids is established. Viscoelastic stress tensor can be represented by a tensor product of magnetic-like vectors. This allows to use the Velikhov-Chandrasekhar criterion of the MRI to predict the elasto-rotational instability (ERI). ERI modes obtained in linear stability and in the experiments are assumed to represent the MRI analogue modes as they are observed in the stable zone according to generalised Rayleigh discriminant.
开普勒体系中的粘弹性泰勒-库埃特不稳定性
采用线性稳定性分析和临界态实验检测方法,研究了粘弹性Taylor-Couette流在开普勒流域中的失稳模式。导出了一种广义瑞利判据,该判据允许将潜在的纯弹性失稳模态区与稳定模态区分开。将粘弹性Taylor-Couette流动的不稳定性与导电流体的磁旋不稳定性(MRI)进行了类比。粘弹性应力张量可以用类磁矢量的张量积表示。这允许使用MRI的Velikhov-Chandrasekhar标准来预测弹性旋转不稳定性(ERI)。根据广义瑞利判别法,假设在线性稳定性和实验中获得的ERI模式代表在稳定区内观察到的MRI模拟模式。
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来源期刊
Geophysical and Astrophysical Fluid Dynamics
Geophysical and Astrophysical Fluid Dynamics 地学天文-地球化学与地球物理
CiteScore
3.10
自引率
0.00%
发文量
14
审稿时长
>12 weeks
期刊介绍: Geophysical and Astrophysical Fluid Dynamics exists for the publication of original research papers and short communications, occasional survey articles and conference reports on the fluid mechanics of the earth and planets, including oceans, atmospheres and interiors, and the fluid mechanics of the sun, stars and other astrophysical objects. In addition, their magnetohydrodynamic behaviours are investigated. Experimental, theoretical and numerical studies of rotating, stratified and convecting fluids of general interest to geophysicists and astrophysicists appear. Properly interpreted observational results are also published.
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