Thermal infrared observations of asteroid (99942) Apophis with Herschel

被引:38
作者
Mueller, T. G. [1 ]
Kiss, C. [2 ]
Scheirich, P. [3 ]
Pravec, P. [3 ]
O'Rourke, L. [4 ]
Vilenius, E. [1 ]
Altieri, B. [4 ]
机构
[1] Max Planck Inst Extraterr Phys, D-85741 Garching, Germany
[2] Hungarian Acad Sci, Res Ctr Astron & Earth Sci, Konkoly Observ, H-1121 Budapest, Hungary
[3] Acad Sci Czech Republ, Inst Astron, CS-25165 Ondrejov, Czech Republic
[4] European Space Agcy, ESAC, Madrid 28691, Spain
关键词
minor planets; asteroids: individual: (99942) Apophis; radiation mechanisms: thermal; techniques: photometric; infrared: planetary systems; PHYSICAL-PROPERTIES; LIGHTCURVE INVERSION; OPTIMIZATION METHODS; EARTH; SHAPE; MAGNITUDE; ITOKAWA; TARGET; CALIBRATION; STANDARDS;
D O I
10.1051/0004-6361/201423841
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The near-Earth asteroid (99942) Apophis is a potentially hazardous asteroid. We obtained far-infrared observations of this asteroid with the Herschel Space Observatory PACS instrument at 70, 100, and 160 mu m. These were taken at two epochs in January and March 2013 during a close-Earth encounter. These first thermal measurements of Apophis were taken at similar phase angles before and after opposition. We performed a detailed thermophysical model analysis by using the spin and shape model recently derived from applying a two-period Fourier series method to a large sample of well-calibrated photometric observations. We found that the tumbling asteroid Apophis has an elongated shape with a mean diameter of 375(-10)(+14)m (of an equal volume sphere) and a geometric V-band albedo of 0.30(-0.06)(+0.05). We found a thermal inertia in the range 250-800 Jm(-2) s(-0.5) K-1 (best solution at Gamma = 600 Jm(-2) s(-0.5) K-1). Which can be explained by a mixture of low-conductivity One regolith with larger rocks and boulders of high thermal inertia on the surface. The thermal inertia, and other similarities with (25143) Itokawa indicate that Apophis might also have a rubble-pile structure. If we combine the new size value with the assumption of an Itokawa-like density and porosity we estimate a mass between 4.4 and 6.2 x 10(10) ke, which is more than 2-3 times larger than previous estimates. We expect that the newly derived properties will influence impact scenario studies and the long-term orbit predictions of Apophis.
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页数:10
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