Experimental demonstration of a homogeneous two-scale dynamo

It has been shown theoretically that homogeneous kinematic dynamo action is possible for many unconfined and confined velocity fields, but a rigorous experimental validation is still lacking. G. O. Roberts [Philos. Trans. R. Soc. London, Ser. A 266, 535 (1970)] proposed a spatially periodic velocity field capable to generate a dynamo, which Busse [Geophys. J. R. Astron. Soc. 42, 437 (1975)] modified by introducing a second length scale larger in order to obtain a solution for a finite domain. Based on a scale separation approach Busse [Springer Proceedings in Physics, Vol. 69 (Springer Verlag, New York, 1992)] proposed a conceptual design for an experimental homogeneous dynamo. An engineering design was developed and a test facility has been set up. This test facility is described and first experimental results confirming dynamo action are presented.

[1]  A. Tilgner A kinematic dynamo with a small scale velocity field , 1997 .

[2]  Paul H. Roberts,et al.  Equations governing convection in earth's core and the geodynamo , 1995 .

[3]  F. Busse,et al.  Laboratory Simulation of Thermal Convection in Rotating Planets and Stars , 1976, Science.

[4]  Lathrop,et al.  Toward a self-generating magnetic dynamo: the role of turbulence , 2000, Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics.

[5]  Gerbeth,et al.  Detection of a flow induced magnetic field eigenmode in the riga dynamo facility , 2000, Physical review letters.

[6]  G. Roberts,et al.  Dynamo action of fluid motions with two-dimensional periodicity , 1972, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[7]  Matthias Rheinhardt,et al.  The Karlsruhe Dynamo Experiment. A Mean Field Approach , 1998 .

[8]  G. Roberts Spatially periodic dynamos , 1970, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.