The linear polarization degree (referred to the scattering plane, P r ) as a function of the solar phase angle, α, of solar system objects is a good diagnostic to understand the scattering properties of their surface materials. We report P r of Phaethon over a wide range of α from 19 • .1 to 114 • .3 in order to better understanding properties of its surface materials. The derived phase-polarization curve shows that the maximum of P r , P max , is >42.4% at α >114 • .3, a value significantly larger than those of the moderate albedo asteroids (P max ∼9%). The phase-polarization curve classifies Phaethon as B-type in the polarimetric taxonomy, being compatible with the spectral property. We compute the geometric albedo, p v , of 0.14 ± 0.04 independently by using an empirical slope-albedo relation, and the derived p v is consistent with previous results determined from mid-infrared spectra and thermophysical modeling. We could not find a fit to the period in our polarimetric data in the range from 0 up to 7.208 hr (e.g., less than twice the rotational period) and found significant differences between our P r during the 2017 approach to the Earth and that of the 2016. These results imply that Phaethon has a region with different properties for light scattering near its orbital pole.Note-UT date is the mid-time of the start and final sequences. φ and α are the angle of the scattering plane and the solar phase angle of the observations, respectively. Texp is exposure time of each frame in seconds and number of sequences. UP, GT, and SP in the column of polarimetric standard stars indicate unpolarized standard stars, fully linear polarized light from the Glan-Taylor prism, and strong polarized standard stars, respectively; chosen from Serkowski (1974), Schmidt et al. (1992), andWolff et al. (1996) for calibrating the instrumental polarization.
RESULTS AND DISCUSSION