There is an optimal size for the delivery of small asteroids from Mars
to the Earth by Yarkovsky thermal drag. Basaltic asteroids with radii
of about 6 m take on the average 185 million years (Myr) for their se
mimajor axes to shrink by 0.52 AU, assuming circular orbits and ignori
ng planetary perturbations and collisions. All other sizes take longer
. Bigger objects are slower because they are more massive, and smaller
objects are slower because they are more isothermal. These results ar
e based on treating the asteroids as spheres and solving the heat cond
uction equation using spherical Bessel functions. The small near-Earth
asteroids show a concentration of sizes in the thermal drag range; th
us some of them may come from Mars as survivors of gravitational mecha
nisms which eliminate them on the 10 Myr timescale. The possible role
of thermal drag in Mars-Earth delivery will remain speculative until i
t is included in numerical integrations of the orbits of small asteroi
ds.