Issue |
A&A
Volume 616, August 2018
|
|
---|---|---|
Article Number | A178 | |
Number of page(s) | 10 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201832721 | |
Published online | 03 September 2018 |
Opposition effect on S-type asteroid (25143) Itokawa
1
Department of Physics and Astronomy, Seoul National University,
1 Gwanak,
Seoul
08826, Republic of Korea
e-mail: mingyeong@kasi.re.kr; ishiguro@astro.snu.ac.kr
2
University of Science & Technology,
Daejeon
34113, Republic of Korea
3
Korea Astronomy and Space Science Institute,
Daejeon
34055, Republic of Korea
Received:
21
January
2018
Accepted:
11
May
2018
Aims. The opposition effect has been detected on solar system bodies such as asteroids and comets. Two mechanisms have been proposed to explain the effect: the shadow-hiding opposition effect (SHOE) and the coherent backscattering opposition effect (CBOE). The Hayabusa asteroid sample return mission provides a unique opportunity to investigate the opposition effect on disk-resolved images of the S-type asteroid (25413) Itokawa at very small phase angles α.
Methods. We made use of the data taken at α = 0.°04–2.°54 using the Asteroid Multi-band Imaging Camera (AMICA) on UT 2005 October 13. Comparing sets of two images taken at different phase angles, we derived the opposition slope parameter (SOE) that characterizes a linear increase in the reflectance I∕F per unit phase angle.
Results. We found that (i) SOE is less dependent on the incidence and emission angles; (ii) the reflectance increases nonlinearly toward the opposition at small angles with α ≲ 1.°4, showing a good correlation between mean I∕F and SOE; and (iii) SOE becomes nearly constant at α ≳ 1.°4 and shows no clear correlation between I∕F and SOE.
Conclusions. From these results, we conjecture that CBOE is dominant at α ≲ 1.°4, while SHOE is dominant at α ≳ 1.°4.
Key words: minor planets, asteroids: general / minor planets, asteroids: individual: Itokawa
© ESO 2018
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