  Space weathering is the generic term used for processes that modify the
optical properties of surfaces of atmosphereless rocky bodies under exposure to
the space environment. The general agreement about the relevance of the effects
of space weathering on the spectral properties of S-complex asteroids fails
when some basic quantitative estimates are attempted. In particular, there is
severe disagreement regarding the typical timescales for significant spectral
reddening to occur, ranging from 1 Myr to 1 Gyr. Generally speaking, the
spectral reddening of an individual object can be considered as the sum of
three terms, one (which is relevant for statistical analyses) depending on the
exposure of the object to space weathering during its lifetime, a second one
due to the original surface composition, and a third one (a "noise" term) due
to the combination of poorly constrained effects (e.g., structure and texture
of the surface). The surface of an asteroid is usually covered by regolith, and
its presence and properties presumably play a critical role in the weathering
processes. In this paper we discuss the role played by collisional evolution in
affecting the spectral properties of asteroids and refreshing the surfaces due
to the formation of ejecta, and the necessity of a simultaneous modeling of
collisions and weathering processes. We introduce a new idea, based on the
possibility of a sort of saturation of the refreshing process whenever a
massive reaccumulation of the impact ejecta takes place. In this case, a
dependence of the overall reddening on the asteroid size should naturally come
out. We show that this conclusion is indeed supported by available main belt
asteroid spectroscopic data.
