We describe a new numerical tool based on the smooth particle hydrodyn
amics (SPH) method which is aimed at modeling impacts and collisions i
nvolving small solid objects. Our goal is to develop a suitable tool f
or the study of strength-dominated interactions between solid bodies.
Although giant impacts have recently received most of the attention, c
ollisions and/or impacts involving small (less-than-or-equal-to 50 km)
objects are (and have been) the most frequent ones. We intend to appl
y this model to such studies as the formation of asteroid families, th
e disruption of ringmoons, the accretion of planetesimals, and spallat
ion from large cratering events. In this first paper in a series, we p
resent all physical and numerical aspects of our model as well as a nu
mber of tests performed in order to validate our method. We adopt a st
rength model and implement a von Mises yielding relation for stresses
beyond the Hugoniot elastic limit. At the lower stresses associated wi
th brittle failure, we use a rate-dependent strength based on the nucl
eation of Weibull flaws. Our model propagates statistical cracks at th
e subparticle scale based on the model of Grady and Kipp (1980) and re
solves real cracks in a resolution-independent manner. Our method ensu
res that increases in resolution do not alter the fracture physics, on
ly the accuracy. The resulting system predicts the shapes, locations,
and velocities of the largest fragments in simulated laboratory impact
events with unprecedented accuracy. (C) 1994 Academic Press, Inc.