Additional mixing between the hydrogen burning shell and the base of t
he convective envelope in stars on their first ascent of the red giant
branch is traditionally considered as a possible cause for the star-t
o-star abundance variations in globular clusters. In the present paper
we model this deep mixing by diffusion. Nuclear kinetics equations co
upled with diffusion terms are solved to follow the evolution of stell
ar surface abundances for isotopes taking part in reactions of the pp-
chains, CNO-, NeNa- and MgAl-cycles. Our task is to reproduce the ''gl
obal anticorrelation'' of [O/Fe] versus [Na/Fe] found recently in glob
ular cluster and halo giants by Kraft et al. (1993) and the correlatio
n of [C/Fe] with M(V) observed in M 92 (Langer et al. 1986). It is sho
wn that both correlations can be accounted for by deep diffusive mixin
g with parameters for mixing depth and rate adjusted individually for
each correlation. The deep mixing in red giants with solar metallicity
is demonstrated to allow the interpretation of anomalous O-17/O-16 an
d O-18/O-16 isotope ratios in S and C asymptotic giant branch stars. I
n the conclusion we propose an observational test for the discussed de
ep mixing.