Mixing a cup of tea and break of centrifugal force 
Possible Duplicate:
Vortex in liquid collects particles in center 

Why when you mix a cup of tea with a teaspoon, tea-craps collect in the center of cup, instead of goes near the walls?
 A: A rotating fluid roughly observes a $v=r\omega$ law where $v$ is the velocity of a fluid element or anything moving with the fluid element, $r$ is the distance from the centre and $\omega$ is the roughly constant angular rotation rate.
So if a large particle like a tea leaf residue is found in the fluid, it should rotate at a speed $v$, given a particular distance. However, such large particles will be more suspect to frictional forces by the viscous tea that reduce the velocity of the particle very quickly. So in order to satisfy $v=r\omega$, it has to collect at the centre of the cup once its velocity is completely reduced to zero.

There is yet another reason why such a particle should float to the centre, but I suspect it has a much smaller contribution. In the rotating frame, there is a centrifugal force acting outward on the large particle. Let's ignore Coriolis forces and look at the effect of only this centrifugal force. Now locally, in a small region around this particle, this is analogous to a gravitational field acting along the surface of the fluid outward to the edge of the cup (the Equivalence Principle). You'd expect the particle to move towards the edge then, but remember that this tea leaf particle is less dense than tea (it floats) and so it should feel a force opposite in direction to the imaginary gravitational field (the centrifugal force), just like a tea leaf particle in a stationary fluid should float upwards against a real vertical gravitational field.
This sort of behaviour is counter-intuitive, but it is actually observed in centrifuges where the suspended particles are less dense than the fluid -- they collect in the center. If you want to check this for yourself without a centrifuge (or if you suspect that friction has a greater role in this), take a helium balloon into a train and you will observe that when the train brakes, while you move forward because of the non-inertial force, the balloon actually inclines backwards! (If the braking is long enough for the air to settle and there are no air currents in the cabin -- agreed, it's not the easiest thing to test)
See here for a more detailed explanation of the balloon example : http://physics101.wordpress.com/2008/11/30/balloons-and-accelerations/
A: The previous life of this question gave an explanation based upon slowing convection, caused by the frictional slowing of the fluid, (slower at the edges), which seems a reasonable possibility. In that case fluid flow is needed because the surface of the fluid is changing because of decreasing angular velocity.
I wonder if surface tension might be involved as well (or instead). Surface tension is modified by the curvature of the surface, and our surface does have curvature that varies as a function of radius. Could this be driving small hydrophobic particles towards the center? However, I think the phenomena is also seen in large ocean votices, with logs caught on the surface, and these objects would be too large to be affected by surface tension gradients.
