2002
DOI: 10.5194/npg-9-171-2002
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On the mean-field theory of the Karlsruhe Dynamo Experiment

Abstract: Abstract. In the Forschungszentrum Karlsruhe an experiment has been constructed which demonstrates a homogeneous dynamo as is expected to exist in the Earth's interior. This experiment is discussed within the framework of meanfield dynamo theory. The main predictions of this theory are explained and compared with the experimental results.

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Cited by 56 publications
(97 citation statements)
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References 19 publications
(15 reference statements)
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“…The crucial induction effect of the fluid motion is then, with respect to the mean magnetic field, described as an anisotropic α-effect. The α-coefficient and related quantities have first been calculated for the Roberts flow [19,20,22,23,25]. In the calculations with the spin generator flow carried out so far, apart from the case of small flow rates, a simplifying but not strictly justified assumption was used.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…The crucial induction effect of the fluid motion is then, with respect to the mean magnetic field, described as an anisotropic α-effect. The α-coefficient and related quantities have first been calculated for the Roberts flow [19,20,22,23,25]. In the calculations with the spin generator flow carried out so far, apart from the case of small flow rates, a simplifying but not strictly justified assumption was used.…”
Section: Introductionmentioning
confidence: 99%
“…Both direct numerical solutions of the induction equation for the magnetic field [12,13,14,15,16,17,18] as well as meanfield theory and solutions of the corresponding equations [19,20,21,22,23,24] have been employed. We focus our attention here on this mean-field approach.…”
Section: Introductionmentioning
confidence: 99%
“…Regarding the kinematic α effect, Childress (1979) found that in steady convection α decreases with increasing R m like R −1/2 m . This result is now understood to be a common feature of steady flows (Rädler et al 2002, Rädler & Brandenburg 2008, and is generally not shared by unsteady (e.g. turbulent) flows (Sur et al 2008).…”
mentioning
confidence: 97%
“…Only in the last days of the last century, in December 1999, after expensive preparations, two dynamos ran successfully with liquid sodium flows, one in Riga (Gailitis et al 2000) and one in Karlsruhe (Müller & Stieglitz 2000. The first one (Riga) is clearly different from a mean-field dynamo, but the second one (Karlsruhe) can be well understood as a meanfield dynamo of α 2 type (see Rädler et al 2002).…”
Section: Laboratory Experimentsmentioning
confidence: 99%