  We consider the inverse problem of recovering an isotropic quasilinear
conductivity from the Dirichlet-to-Neumann map when the conductivity depends on
the solution and its gradient. We show that the conductivity can be recovered
on an open subset of small gradients, hence extending a partial result to all
real analytic conductivities. We also recover non-analytic conductivities with
additional growth assumptions along large gradients. Moreover, the results hold
for non-homogeneous conductivities if the non-homogeneous part is assumed
known.
