JpGU-AGU Joint Meeting 2020

Presentation information

[J] Poster

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS27] Geophysical fluid dynamics-Transfield approach to geoscience

convener:Keita Iga(Atmosphere and Ocean Research Institute, The University of Tokyo), Shigeo Yoshida(Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University), Takatoshi Yanagisawa(Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology), Hidenori AIKI(Nagoya University)

[MIS27-P03] Influence of side-wall Hartmann braking in a liquid metal convection under a horizontal magnetic field

*Takatoshi Yanagisawa1, Koki Sawada2, Yuji Tasaka2, Takehiro Miyagoshi3, Ataru Sakuraba4 (1.Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology, 2.Faculty of Engineering, Hokkaido University, 3.Research Institute for Value-Added-Information Generation, Japan Agency for Marine-Earth Science and Technology, 4.Faculty of Science, University of Tokyo)

Keywords:magnetoconvection, Hartmann boundary layer, roll-like structure

The effect of magnetic field is important for flows occurring in liquid metals. For phenomena confined by solid boundaries, the existence of side wall is also essential. We performed both laboratory experiments and numerical simulations on Rayleigh-Benard convection with a liquid metal as the test fluid under a strong horizontal magnetic field to elucidate influence of side-wall Hartmann braking on the phenomena. Vessels with different length in the direction of magnetic field were examined to modify the influence. In the laboratory experiments, horizontal velocity profiles were measured by ultrasonic velocity profiler to observe behavior of the convection and to quantify it. It was confirmed that there are quasi-two-dimensional rolls aligned parallel to the magnetic field because of sufficiently strong magnetic field and the magnitude of convection was characterized as variation of Reynolds number with respect to Chandrasekhar number, which is the ration of Lorenz force to the viscous damping. Scaling law describing the variation was derived with assumption of balance between buoyancy given by vertical temperature difference and side-wall Hartmann braking, which is viscous dissipation due to thinning of side-wall boundary layer perpendicular to the magnetic field (Hartmann layer) by the Lorentz force. It is expected that as the length scale in the magnetic field becomes narrower, the influence of Hartmann braking becomes stronger. The variations for different Rayleigh number and the length scale were collapsed into a unified curve by normalization according to the scaling law at conditions of relatively strong magnetic field.