Forced reconnection in a current-carrying two-dimensional resistive ma
gneto-fluid is explored in a slab geometry. The time development of th
e two-dimensional processes that occur is studied numerically. Perturb
ation of the wall during a few Alfven times generate ideal megnetohydr
odynamics (MHD) waves that propagate towards the neutral layer and gen
erate a current layer along it. The formation of the current sheet nea
r the X point and the vortex motion inside the island are analysed in
the nonlinear regime. In this phase the current in the X point of the
generated island grows exponentially with time while it is still gover
ned by ideal MHD. After having reached a maximum the current decreases
sharply. This maximum and the subsequent decrease are determined by r
esistivity and the narrowing of the local current profile, which is an
ideal effect. The current distribution becomes that of a sheet curren
t, especially for low values of the resistivity. Eventually a quasi-st
ationary state is reached in which current and vorticity are localized
along the separatrix.