Chin. Phys. Lett.  2014, Vol. 31 Issue (03): 030401    DOI: 10.1088/0256-307X/31/3/030401
GENERAL |
Incompressible Magnetohydrodynamic Kelvin–Helmholtz Instability with Continuous Profiles
ZHAO Kai-Ge1, WANG Li-Feng2,3, YE Wen-Hua2,3,4, WU Jun-Feng2**, LI Ying-Jun1**
1State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Beijing 100083
2Institute of Applied Physics and Computational Mathematics, Beijing 100094
3HEDPS, Center for Applied Physics and Technology, Peking University, Beijing 100871
4Department of Physic, Zhejiang University, Hangzhou 310027
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ZHAO Kai-Ge, WANG Li-Feng, YE Wen-Hua et al  2014 Chin. Phys. Lett. 31 030401
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Abstract Effects of a continuous magnetic field in the direction of streaming on the incompressible Kelvin–Helmholtz instability (KHI) are investigated by solving the linear ideal magnetohydrodynamic equations. It is found that the frequency of the KHI is not influenced by the magnetic field. The magnetic field strength effect decreases the linear growth of the KHI, while the magnetic field gradient scale length effect increases its linear growth. The KHI can even be completely suppressed when the magnetic field is strong enough. The linear growth rate approaches a maximum when the magnetic field gradient scale length is large enough.
Received: 12 August 2013      Published: 28 February 2014
PACS:  04.30.Tv (Gravitational-wave astrophysics)  
  47.20.Ft (Instability of shear flows (e.g., Kelvin-Helmholtz))  
  52.30.Cv (Magnetohydrodynamics (including electron magnetohydrodynamics))  
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https://cpl.iphy.ac.cn/10.1088/0256-307X/31/3/030401       OR      https://cpl.iphy.ac.cn/Y2014/V31/I03/030401
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ZHAO Kai-Ge
WANG Li-Feng
YE Wen-Hua
WU Jun-Feng
LI Ying-Jun
[1] Chandrasekhar S 1961 Hydrodynamic and Hydromagnetic Stability (London: Oxford University Press)
[2] Lindl J D et al 2004 Phys. Plasmas 11 339
[3] He X T and Zhang W Y 2007 Eur. Phys. J. D 44 227
[4] Wang L F et al 2010 Phys. Plasmas 17 122706
[5] Wang L F, Ye W H, Don W S, Sheng Z M, Li Y J and He X T 2010 Phys. Plasmas 17 122308
[6] Spolaore N et al 2009 Phys. Rev. Lett. 102 165001
[7] Boozer A H 2005 Rev. Mod. Phys. 76 1071
[8] Uberoi C 1984 J. Geophys. Res. 89 5652
[9] Gamexo V N et al 2003 Science 299 77
[10] Wang L F, Xue C, Ye W H and Li Y J 2009 Phys. Plasmas 16 112104
[11] Wang L F, Ye W H and Li Y J 2009 Europhys. Lett. 87 54005
[12] Wang L F et al 2010 Phys. Plasmas 17 042103
[13] Ye W H et al 2011 Phys. Plasmas 18 022704
[14] Miura A 1982 Phys. Rev. Lett. 49 779
[15] Miura A and Pritchett P L 1982 J. Geophys. Res. 87 7431
[16] Nakamura T K M and Fujimoto M 2008 Phys. Rev. Lett. 101 165002
[17] Walker J S, Talmage G, Brown S H and Sondergaard N A 1993 Phys. Fluids A 5 1466
[18] Wang L F et al 2009 Commun. Theor. Phys. 52 694
[19] Wang L F et al 2010 Phys. Plasmas 17 122308
[20] Wang L F et al 2009 Chin. Phys. Lett. 26 074704
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