An attempt is made to infer the structure of the solar convection zone
from observed p-mode frequencies of solar oscillations. The different
ial asymptotic inversion technique is used to find the sound speed in
the solar envelope. It is found that envelope models which use the Can
uto-Mazzitelli (CM) formulation for calculating the convective flux gi
ve significantly better agreement with observations than models constr
ucted using the mixing length formalism. This inference can be drawn f
rom both the scaled frequency differences and the sound speed differen
ce. The sound speed in the CM envelope model is within 0.2% of that in
the Sun except in the region with r>0.99R. The envelope models are ex
tended below the convection zone, to find some evidence for the gravit
ational settling of helium beneath the base of the convection zone. It
turns out that for models with a steep composition gradient below the
convection zone, the convection zone depth has to be increased by abo
ut 6 Mm in order to get agreement with helioseismic observations.