2013
DOI: 10.1016/j.crhy.2012.12.002
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Magnetic induction maps in a magnetized spherical Couette flow experiment

Abstract: soumis au Comptes Rendus PhysiqueInternational audienceThe DTS experiment is a spherical Couette flow experiment with an imposed dipolar magnetic field. Liquid sodium is used as a working fluid. In a series of measurement campaigns, we have obtained data on the mean axisymmetric velocity, the mean induced magnetic field and electric potentials. All these quantities are coupled through the induction equation. In particular, a strong omega-eff ect is produced by di fferential rotation within the fluid shell, ind… Show more

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Cited by 12 publications
(29 citation statements)
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“…Following earlier works [8,10], we collect ultrasound Doppler velocity profiles, electric potential measurements, global torque data, and measurements of the induced magnetic field inside the sodium layer, to reconstruct meridional maps of the mean flow and magnetic field at a given Rm, taking into account the link established by the induction equation. But we further constrain these fields by analyzing the response of the fluid shell to a time-periodic magnetic field, as in Frick et al [4].…”
mentioning
confidence: 99%
“…Following earlier works [8,10], we collect ultrasound Doppler velocity profiles, electric potential measurements, global torque data, and measurements of the induced magnetic field inside the sodium layer, to reconstruct meridional maps of the mean flow and magnetic field at a given Rm, taking into account the link established by the induction equation. But we further constrain these fields by analyzing the response of the fluid shell to a time-periodic magnetic field, as in Frick et al [4].…”
mentioning
confidence: 99%
“…The m = 0 data and data errors are acquired and processed as described by Nataf [21]. The main difference is that we focus here on data for a rotation rate f = ±9 Hz, instead of ±3 Hz in [21].…”
Section: Axisymmetric Data Acquisition and Processingmentioning
confidence: 99%
“…In an effort to evaluate the contributions of turbulent fluctuations to the mean large-scale magnetic field in the DTS experiment, Nataf [21] inverted simultaneously mean velocity and magnetic data in order to evaluate by difference the part of the mean magnetic field that is not induced by the mean velocity field. He also evaluated an upper bound for the contribution of the fluctuations to the mean field by mapping the amplitude of magnetic and velocity fluctuations.…”
Section: Introductionmentioning
confidence: 99%
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“…However, for our current problem, a more simple and lighter method makes use of the fact that the spherical harmonics form a natural basis for both the acoustic modes and the flow field. More specifically, the azimuthal velocity field θ Ω θ θ = ϕ U r r r ( , ) ( , ) sin can be written as [12]:…”
Section: Semi-spectral Bayesian Inversionmentioning
confidence: 99%