We consider the irreversible nucleation and growth of two-dimensional islan
ds during submonolayer deposition in the regime of large island sizes. A qu
asihydrodynamic analysis of rate equations for island densities yields an o
rdinary differential equation (ODE) for the scaling function describing the
island size distribution. This ODE involves the scaling function for the d
ependence on island size of ''capture numbers'' describing the aggregation
of diffusing adatoms. The latter is determined via a quasihydrodynamic anal
ysis of rate equations for the areas of "capture zones" surrounding islands
. Alternatively, a more complicated analysis yields a partial differential
equation (PDE) for the scaling function describing the joint probability di
stribution for island sizes and capture zone areas. Then, applying a moment
analysis to this PDE, we obtain refined versions of the above ODE's, toget
her with a third equation for the variance of the cell area distribution (f
or islands of a given size). The key nontrivial input to the above equation
s is a detailed characterization of nucleation. We analyze these equations
for a general formulation of nucleation, as well as for an idealized pictur
e considered previously, wherein nucleated islands have capture zones lying
completely within those of existing islands.