2017
DOI: 10.1016/j.icarus.2016.11.003
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Refining the asteroid taxonomy by polarimetric observations

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Cited by 59 publications
(76 citation statements)
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References 54 publications
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“…We found for Bennu Ψ = 6.083 ± 0.266 and a corresponding formal solution for the albedo of 0.059 ± 0.003. This value, to be confirmed when a better sampling of the phase-polarisation curve is available, fits nicely the value found for the F-class by Belskaya et al (2017), namely 0.058 ± 0.011. The same authors found for the B-class an average albedo of 0.083 ± 0.034.…”
Section: Datesupporting
confidence: 87%
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“…We found for Bennu Ψ = 6.083 ± 0.266 and a corresponding formal solution for the albedo of 0.059 ± 0.003. This value, to be confirmed when a better sampling of the phase-polarisation curve is available, fits nicely the value found for the F-class by Belskaya et al (2017), namely 0.058 ± 0.011. The same authors found for the B-class an average albedo of 0.083 ± 0.034.…”
Section: Datesupporting
confidence: 87%
“…For the vast majority of asteroids the polarisation changes its sign (i.e., becomes perpendicular to the scattering plane) at phase-angles 20 • (the "inversion angle" αinv). However, in the case of the F-class asteroids, the inversion angle occurs at the distinctly lower phase-angle of ∼ 16 • (Belskaya et al 2017). Furthermore, the slope of the polarimetric curve around the inversion angle tends to be substantially steeper for F-class asteroids with respect to other taxonomic classes.…”
Section: Introductionmentioning
confidence: 91%
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“…The polarimetric observation results of 86 asteroids using the Bus-DeMeo taxonomy were referred from (Belskaya et al 2017;Cellino et al 2015;Cellino et al 2016;Gil-Hutton, Cellino, & Bendjoya 2014); the radar values for 74 classified asteroids were obtained from Neese, Benner, & Ostro (2012). The polarimetric and radar values of the classified asteroids are shown in figures 7 and 8, respectively.…”
Section: Number Numbermentioning
confidence: 99%
“…The primary constituents of cometary dust are silicates (mainly in the form of olivine and pyroxene), carbonaceous materials (amorphous carbon and organics), Fe-bearing sulfides, and ice (Levasseur-Regourd et al 2018). Unlike asteroids, the optical properties of which are largely differentiated with respect to heliocentric distance (DeMeo & Carry 2014;Belskaya et al 2017), comets seem to possess fairly homogeneous bulk optical properties with a low geometric albedo of ∼0.04 (Lamy et al 2004), showing a nearly uniform distribution on the polarimetric phase curves, regardless of dynamical classes (Kwon et al 2017). However, any difference in a comet might be expected if we consider the grain properties with depth in the nucleus, perhaps as a result of mainly solar irradiation on the outer layers.…”
Section: Change In Composition Of Dust Particlesmentioning
confidence: 99%