We study the chemical evolution of population I and population II secondari
es in cataclysmic variables (CVs) assuming that during nova explosions a pa
rt of the high metallicity nova ejecta is intercepted by the secondary and
mixed into its convective envelope. We derive analytic expressions for the
chemical composition of the envelope of the secondary as a function of the
chemical composition of the nova ejecta X-i,X-ej and the cross-section of t
he secondary sigma. For population I CVs we find that the increase of the m
etallicity of the secondary is comparable to its initial metallicity only i
f sigma is larger by an order of magnitude than the geometrical cross-secti
on. A significant accumulation is therefore possible only in those species
that are highly overabundant in the nova ejecta. Because the changes in the
abundances of even those species depend strongly on the poorly known cross
-section a, the predictive power of our model is weak for population I CVs
as long as sigma is not well determined. Tn the case of population II CVs t
he accumulation of heavy elements by this process dominates over the initia
l metallicity of the secondary even for values of sigma that are smaller by
an order of magnitude than the geometrical cross-section. Thus, within a s
hort time after turn-on of mass transfer, the relative metal abundances in
the envelope of the secondary reflect those in the nova ejecta. This is nea
rly independent of the cross-section sigma.