We present a minimalistic approach to simulations of force transmission thr
ough granular systems. We start from a configuration containing cohesive (t
ensile) contact forces and use an adaptive procedure to find the stable con
figuration with no tensile contact forces. The procedure works by sequentia
lly removing and adding individual contacts between adjacent beads, while t
he bead positions are not modified. In a series of two-dimensional realizat
ions, the resulting force networks are shown to satisfy a linear constraint
among the three components of average stress, as anticipated by recent the
ories. The coefficients in the linear constraint remain nearly constant for
a range of shear loadings up to about 0.6 of the normal loading. The spati
al distribution of contact forces shows strong concentration along "force c
hains." The probability of contact forces of magnitude f shows an exponenti
al falloff with f. The response to a local perturbing force is concentrated
along two characteristic rays directed downward and laterally.