A systematic study of the motion backward and forward in time from a u
niform distribution of bodies entering a planet's Hill sphere yields a
mapping of the contribution to the planet's rotation from planetesima
ls as a function of their source in heliocentric orbital element space
. The mapping allows determination of the contribution to rotation fro
m any assumed distribution of heliocentric planetesimal orbits. For ex
ample, it can systematically reproduce earlier results from Monte-Carl
o studies of contributions to rotational angular momentum. With our me
thod of calculation, contributions to planetary rotation can be interp
reted in terms of the arrival geometries at the planet's Hill sphere a
nd the subsequent two-body motion inside the Hill sphere leading to im
pact. Prograde rotation is strongly favored if a planet grows in a rel
atively quiescent population of planetesimals with accretion nibbling
at the edges of its feeding zone. However, if the impacting population
were dominated by large bodies with high relative velocity, the direc
tion and magnitude of rotation would be random. (C) 1997 Academic Pres
s.