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Abstracts - KTH Mechanics

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Generation of magnetic fields by turbulent flows<br />

S. Fauve ∗ ,F.Pétrélis †<br />

The generation of a magnetic field by the flow of an electrically conducting fluid,<br />

i.e. the dynamo effect, has been first considered to explain the origin of the magnetic<br />

fields of planets, stars and galaxies. It has been also studied in relation with several<br />

applied problems such as liquid metal cooling of nuclear reactors, liquid metal<br />

electromagnets and instabilities in toroidal plasmas. Magnetic field generation by<br />

laminar flows is fairly well understood and dynamos generated by simple but clever<br />

flow geometries have been successfully observed in experiments performed a few years<br />

ago in Karlsruhe and Riga.<br />

However, the effect of turbulence on dynamo threshold and saturation still involves<br />

many open problems. We have shown that small scale turbulent fluctuations<br />

only slightly modify the dynamo threshold predicted as if the mean flow were acting<br />

alone, in agreement with the Karlsrhue and Riga experimental observations 1 . On<br />

the contrary, large scale fluctuations of eddies generating the field can strongly inhibit<br />

the dynamo effect, as shown in an analytically tractable example. Thus, the<br />

behaviour of the dynamo threshold of strongly turbulent flows as a function of the kinetic<br />

Reynolds number, is still an open problem involving many conflicting statements<br />

in the literature.<br />

The nonlinearly saturated dynamo regime also depends on the Reynolds number<br />

of the flow generating the magnetic field. We show that different scaling laws can<br />

be obtained for the magnetic energy generated in the vicinity of the threshold 2 and<br />

compare them to the values measured in Karlsruhe and Riga. The importance of<br />

the Coriolis force, crucial for astrophysical or geophysical dynamos, is also shortly<br />

discussed.<br />

Dynamos generated by strongly turbulent flows of liquid metal as well as astrophysical<br />

or geophysical dynamos, cannot be studied with direct numerical simulations<br />

of the equations of magnetohydrodynamics in a realistic parameter range. Progress in<br />

this direction thus strongly relies on experimental observations and several groups in<br />

the world are trying to generate a turbulent dynamo 3 . We will shortly review these<br />

efforts and show how the study of fluctuations and transport of a magnetic field by<br />

the flow of a liquid metal can give insights in the relevant mechanisms of turbulent<br />

dynamos 4 5 .<br />

∗ Laboratoire de Physique Statistique, Ecole Normale Supérieure, 24 rue Lhomond 75005 Paris,<br />

France.<br />

† Laboratoire de Physique Statistique, Ecole Normale Supérieure, 24 rue Lhomond 75005 Paris,<br />

France.<br />

1 Fauve and Pétrélis, Peyresq Lectures on Nonlinear Phenomena, Ed. J-A Sepulchre, World<br />

Scientific 2, 1 (2003).<br />

2 Pétrélis and Fauve, Eur. Phys. J. B 22, 273 (2001).<br />

3 Fauve and Lathrop, Fluid Dynamics and Dynamos in Astrophysics and Geophysics, A. Soward<br />

et al., Eds. 393 (2005).<br />

4 Bourgoin et al., Phys. Fluids 14, 3046 (2002).<br />

5 Pétrélis et al., Phys. Rev. Lett. 90, 174501 (2003).<br />

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