Abstract:
Based on the solution of the hydrodynamic equations and Maxwell's equations, we show that an external quasi-homogeneous magnetic field leads to the emergence of a secondary electric field that is resulted from a nonlinear effect over magnetic potential $\mathbf A$. This field is proved to exist in the region with a depth of $\delta/2$, where $\delta$ is the London penetration depth. The hydrodynamic flow velocity is estimated.
Keywords:Maxwell equations, penetration depth, magnetic field, electric field, nonlinear effect.
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