학술논문
Color, Composition, and Thermal Environment of Kuiper Belt Object (486958) Arrokoth
Document Type
Working Paper
Author
Grundy, W. M.; Bird, M. K.; Britt, D. T.; Cook, J. C.; Cruikshank, D. P.; Howett, C. J. A.; Krijt, S.; Linscott, I. R.; Olkin, C. B.; Parker, A. H.; Protopapa, S.; Ruaud, M.; Umurhan, O. M.; Young, L. A.; Ore, C. M. Dalle; Kavelaars, J. J.; Keane, J. T.; Pendleton, Y. J.; Porter, S. B.; Scipioni, F.; Spencer, J. R.; Stern, S. A.; Verbiscer, A. J.; Weaver, H. A.; Binzel, R. P.; Buie, M. W.; Buratti, B. J.; Cheng, A.; Earle, A. M.; Elliott, H. A.; Gabasova, L.; Gladstone, G. R.; Hill, M. E.; Horanyi, M.; Jennings, D. E.; Lunsford, A. W.; McComas, D. J.; McKinnon, W. B.; McNutt Jr., R. L.; Moore, J. M.; Parker, J. W.; Quirico, E.; Reuter, D. C.; Schenk, P. M.; Schmitt, B.; Showalter, M. R.; Singer, K. N.; Weigle II, G. E.; Zangari, A. M.
Source
Subject
Language
Abstract
The outer Solar System object (486958) Arrokoth (provisional designation 2014 MU$_{69}$) has been largely undisturbed since its formation. We study its surface composition using data collected by the New Horizons spacecraft. Methanol ice is present along with organic material, which may have formed through radiation of simple molecules. Water ice was not detected. This composition indicates hydrogenation of carbon monoxide-rich ice and/ or energetic processing of methane condensed on water ice grains in the cold, outer edge of the early Solar System. There are only small regional variations in color and spectra across the surface, suggesting Arrokoth formed from a homogeneous or well-mixed reservoir of solids. Microwave thermal emission from the winter night side is consistent with a mean brightness temperature of 29$\pm$5 K.
Comment: 31 pages, 8 figures
Comment: 31 pages, 8 figures