Thermal inertia of main belt asteroids smaller than 100 km from IRAS data
Marco Delbo (OCA), Paolo Tanga (OCA)

TL;DR
This study estimates the thermal inertia of main belt asteroids smaller than 100 km using IRAS data, filling a size gap and refining the correlation between asteroid size and thermal properties.
Contribution
It provides new thermal inertia estimates for 100 km MBAs, improving understanding of regolith development and impact processes across asteroid sizes.
Findings
Confirmed inverse correlation between thermal inertia and size.
Discriminated spin vector solutions for some asteroids.
Supported theoretical predictions for asteroid spin states.
Abstract
Recent works have shown that the thermal inertia of km-sized near-Earth asteroids (NEAs) is more than two orders of magnitude higher than that of main belt asteroids (MBAs) with sizes (diameters) between 200 and 1,000 km. This confirms the idea that large MBAs, over hundreds millions of years,have developed a fine and thick thermally insulating regolith layer, responsible for the low values of their thermal inertia, whereas km-sized asteroids, having collisional lifetimes of only some millions years, have less regolith, and consequently a larger surface thermal inertia. Because it is believed that regolith on asteroids forms as a result of impact processes, a better knowledge of asteroid thermal inertia values and its correlation with size, taxonomic type, and density can be used as an important constraintfor modeling of impact processes on asteroids. However, our knowledge of…
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