arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1210.1990physics.flu-dynphysics.geo-ph
收藏

磁化球库埃特流实验中的Magnetic induction图

Magnetic induction maps in a magnetized spherical Couette flow experiment

Henri-Claude Nataf

摘要:

该实验是一个球形库埃特流实验与强加的偶极磁场。液体钠被用作工作流体。在一系列的测量活动中,我们获得了平均轴对称速度,平均感应磁场和电势的数据。所有这些量都通过感应方程耦合起来。特别是,一个强大的欧米茄效应是由不同的旋转内的流体壳,诱导一个显着的方位角磁场。利用简单的球形几何的实验,我扩大到勒让德多项式的方位角和tendronal字段和推导出的表达式,所有的测量速度场的径向函数为每个谐波度。对于小的磁雷诺数Rm的关系是线性的,和方位角和双曲方程解耦。选择一组的测量为一个给定的旋转频率的内球(Rm = 9.4),我同时反演的速度和磁性数据,从而重建的方位角和双曲场内的流体壳。结果表明,测量的内部一致性良好,并指出,湍流非轴对称波动不贡献显着的轴对称磁感应强度。

英文摘要:

The 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, inducing a significant azimuthal magnetic field. Taking advantage of the simple spherical geometry of the experiment, I expand the azimuthal and meridional fields into Legendre polynomials and derive the expressions that relate all measurements to the radial functions of the velocity field for each harmonic degree. For small magnetic Reynolds numbers Rm the relations are linear, and the azimuthal and meridional equations decouple. Selecting a set of measurements for a given rotation frequency of the inner sphere (Rm = 9.4), I invert simultaneously the velocity and the magnetic data and thus reconstruct both the azimuthal and the meridional fields within the fluid shell. The results demonstrate the good internal consistency of the measurements, and indicate that turbulent non-axisymmetric fluctuations do not contribute significantly to the axisymmetric magnetic induction.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑