Space Weathering

By David Polishook – Tel-Aviv University

 

            Differences between the spectral types of NEAs and MBAs that have the same origins (Chapman 2004) led to the conclusion that NEAs are not different from MBAs, but rather represent an evolutionary stage of known taxonomies. Binzel et al. (1996), found a continuum distribution of the 1μm band strength in asteroid spectra, between the relatively shallow band depths of the S-type MBAs asteroids to the relatively deep (therefore interpreted as fresh) Q-type NEAs. From this, it seems that the small Q-type NEAs (the largest with a diameter of ~5 km) could be understood as fragments, with freshly exposed surfaces, originating from larger, S-type, old MB asteroids. According to this theory, the "old" objects have been exposed to "space weathering", a variety of effects such as solar wind, cosmic rays and micrometeorite bombardment that modify the optical characteristic of their surfaces (Clark et al. 2002). The effects of space weathering have been measured on lunar soil and on grained meteorites that was exposed to extreme radiation bombardment in the laboratory. Images with transmission electron microscopy (TEM) of individual lunar soil grains suggest that the different causes for the "space weathering" effect are vaporizing minerals on the surface. When these minerals sink back to the surface, they are altered in a way that rims of Fe metal particles are abundant on the "weathered" surface. These metal particles change the reflectance spectra of the asteroid to appear redder and darker as they obscure the spectral properties of the minerals below them.

            Binary asteroids formed from a disrupted single object might present fresh surfaces that were unexposed to space weathering on the specific body section where the disruption took place. This is true only if the disruption time is shorter than the timescale of space weathering. In this way, the time of disruption of the progenitor asteroid into a binary system can be determined. In addition, observing fresh areas allows a glimpse to the asteroids' interior and a possibility to compare it with the exposed material on the surface. Therefore, binary asteroids are good candidates for finding color variation as the asteroid rotates and for linking between different aspects of asteroids evolution such as disruption and space weathering effects.