Phase reddening on asteroid Bennu from visible and near-infrared spectroscopy
S. Fornasier, P. H. Hasselmann, J. D. P Deshapriya, M. A. Barucci, B., E. Clark, A. Praet, V. E. Hamilton, A. Simon, J-Y. Li, E. A. Cloutis, F., Merlin, X-D. Zou, D. S. Lauretta

TL;DR
This study analyzes how Bennu's spectral slope varies with phase angle using OSIRIS-REx data, revealing a monotonic, wavelength-dependent phase reddening effect that varies across surface features and is consistent with fine, rough particles.
Contribution
First detailed investigation of spectral phase reddening on Bennu across a wide phase angle range using in-situ spectra, highlighting surface micro-roughness effects.
Findings
Spectral slope increases linearly with phase angle up to 90°
Phase reddening coefficient is 0.00044 μm$^{-1}$ deg$^{-1}$ in 0.55-2.5 μm range
Surface regions like Nightingale show steeper reddening, indicating fine material presence
Abstract
The NASA mission OSIRIS-REx has been observing near-Earth asteroid (101955) Bennu in close proximity since December 2018. In this work, we investigate spectral phase reddening -- that is, the variation of spectral slope with phase angle -- on Bennu using spectra acquired by the OSIRIS-REx Visible and InfraRed Spectrometer (OVIRS) covering a phase angle range of 8-130. We investigate this process at the global scale and for some localized regions of interest (ROIs), including boulders, craters, and the designated sample collection sites of the OSIRIS-REx mission. Bennu has a globally negative spectra slope, which is typical of B-type asteroids. The spectral slope gently increases in a linear way up to a phase angle of 90, where it approaches zero. The spectral phase reddening is monotonic and wavelength-dependent with highest values in the visible range. Its coefficient…
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