Polarimetric Study of Near-Earth Asteroid (1566) Icarus

TL;DR

This study presents polarimetric observations of near-Earth asteroid (1566) Icarus, revealing its surface properties, albedo, and roughness, and compares these findings with other celestial bodies and laboratory samples.

Contribution

First polarimetric analysis of asteroid Icarus at large phase angles, providing insights into its surface composition and physical properties.

Findings

Maximum polarization degree is around 7.3% at 124° phase angle.

Derived geometric albedo of 0.25 consistent with Q-type asteroids.

Surface likely has large macroscopic roughness and paucity of small grains.

Abstract

We conducted a polarimetric observation of the fast-rotating near-Earth asteroid (1566) Icarus at large phase (Sun-asteroid-observer's) angles $\alpha$= 57 deg--141deg around the 2015 summer solstice. We found that the maximum values of the linear polarization degree are $P_\mathrm{max}$=7.32$\pm$0.25 % at phase angles of $\alpha_\mathrm{max}$=124$\pm$8 deg in the $V$-band and $P_\mathrm{max}$=7.04$\pm$0.21 % at $\alpha_\mathrm{max}$=124$\pm$6 deg in the $R_\mathrm{C}$-band. Applying the polarimetric slope-albedo empirical law, we derived a geometric albedo of $p_\mathrm{V}$=0.25$\pm$0.02, which is in agreement with that of Q-type taxonomic asteroids. $\alpha_\mathrm{max}$ is unambiguously larger than that of Mercury, the Moon, and another near-Earth S-type asteroid (4179) Toutatis but consistent with laboratory samples with hundreds of microns in size. The combination of the maximum polarization degree and the geometric albedo is in accordance with terrestrial rocks with a diameter of several hundreds of micrometers. The photometric function indicates a large macroscopic roughness. We hypothesize that the unique environment (i.e., the small perihelion distance $q$=0.187 au and a short rotational period of $T_\mathrm{rot}$=2.27 hours) may be attributed to the paucity of small grains on the surface, as indicated on (3200) Phaethon.