While the solar convection zone is very well mixed by its turbulent motions
, chemical composition gradients build up in the radiative interior due to
microscopic diffusion and settling, and to nuclear burning. Standard models
, which ignore any type of macroscopic transport, cannot explain the deplet
ion of lithium in solar-type stars, as they evolve; neither do they account
for the observed profile of molecular weight at the base of the solar conv
ection zone.
Such macroscopic transport can be achieved through thermally driven meridia
n currents, through turbulent diffusion generated by differential rotation
and possibly through gravity waves. These processes transport also angular
momentum, and therefore the internal rotation profile of the Sun provides a
crucial test for their relative importance. So does also the behavior of t
idally locked binaries, which appear to destroy less lithium than single st
ars of the same mass.