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Magnetically Induced Rotating Rayleigh-Taylor Instability
Published on: March 3, 2017
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Dynamo Action in a Quasi-Keplerian Taylor-Couette Flow.
Anna Guseva1, Rainer Hollerbach2, Ashley P Willis3
1University of Bremen, Center of Applied Space Technology and Microgravity (ZARM), 28359 Bremen, Germany.
Physical Review Letters
|November 4, 2017
Summary
This study demonstrates a finite-amplitude dynamo in a quasi-Keplerian flow. Mutually sustaining turbulence and magnetic fields emerge, increasing angular momentum transport via Maxwell stresses.
Area of Science:
- Fluid dynamics
- Magnetohydrodynamics
- Plasma physics
Background:
- Taylor-Couette flow with quasi-Keplerian rotation is typically Rayleigh stable.
- Nonmagnetic systems in this regime lack kinematic dynamo action.
Purpose of the Study:
- To numerically investigate dynamo action in a quasi-Keplerian Taylor-Couette flow.
- To determine if turbulence and magnetic fields can mutually sustain each other.
Main Methods:
- Numerical computation of electrically conducting fluid flow.
- Utilizing a quasi-Keplerian rotation rate: Ω_{o}/Ω_{i}=(r_{o}/r_{i})^{-3/2}.
- Simulations performed at Reynolds number (Re) = 10^4 and magnetic Reynolds number (Rm) = 10^5.
Main Results:
- Demonstrated the existence of a finite-amplitude dynamo.
- Observed mutually sustaining turbulence and magnetic fields.
- Significant increase in outward angular momentum transport.
Conclusions:
- A dynamo can exist in this stable, nonmagnetic configuration.
- Maxwell stresses dominate angular momentum transport over Reynolds stresses.
- Finite-amplitude dynamos can arise from specific initial conditions.
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