In general, the Stokes-Einstein (SE) equation is well accepted for melts. In the supercooled melt a decoupling of diffusivity and viscosity around the critical temperature Tc of the mode coupling theory is observed. The authors measured simultaneously the P32 and Co57 diffusion in the supercooled melt of the Pd43Cu27Ni10P20 alloy from 573 up to 640K using the radiotracer technique. They found that P and Co have similar diffusivities and compared them to viscosity data using SE equation. This shows that the time scales of Co and P diffusions are decoupled by up to two orders of magnitude from time scales of viscous flow in the supercooled state.

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