  A deposition process with particles having realistic intermediate stickiness
is studied in 2+1 dimensions. At each stage of the deposition process, for any
given configuration, a newly depositing particle gives rise to allowed set of
configurations that are vastly larger than those for deposition of a mixture of
purely non-sticky (random like) and purely sticky (ballistic like) particles.
We obtain scaling behavior and demonstrate collapse of scaled data for surface
width and porosity. Scaling of conductivity, when a porous structure thus
formed, is saturated with conductive fluid, e.g. brine, is studied. The results
obtained are in good agreement with Archie's law for porous sedimentary rocks.
