Asteroids seen by JWST-MIRI: Radiometric size, distance, and orbit constraints

被引:2
|
作者
Mueller, T. G. [1 ]
Micheli, M. [2 ]
Santana-Ros, T. [3 ,4 ]
Bartczak, P. [5 ,6 ]
Oszkiewicz, D. [5 ]
Kruk, S. [1 ]
机构
[1] Max Planck Inst Extraterr Phys, Giessenbachstr,Postfach 1312, D-85741 Garching, Germany
[2] ESA NEO Coordinat Ctr, Largo Galileo Galilei 1, I-00044 Frascati, RM, Italy
[3] Univ Alicante, Dept Fis Ingn Sistemas & Teoria Senal, Carr San Vicente del Raspeig S-N, San Vicente Del Raspeig 03690, Alicante, Spain
[4] Univ Barcelona IEEC UB, Inst Ciencies Cosmos ICCUB, Carrer Marti & Franques 1, Barcelona 08028, Spain
[5] Adam Mickiewicz Univ, Astron Observ Inst, Fac Phys, Sloneczna 36, PL-60286 Poznan, Poland
[6] Univ Alicante, Inst Univ Fis Aplicada Ciencias & Tecnol IUFACyT, Ctra San Vicente del Raspeig S-N, San Vicente Del Raspeig 03690, Alicante, Spain
基金
美国国家航空航天局; 美国国家科学基金会; 欧盟地平线“2020”;
关键词
minor planets; asteroids; general; individual; (10920); infrared; planetary systems; techniques; photometric; radiation mechanisms; thermal; WEBB-SPACE-TELESCOPE; THERMAL PHYSICS; PHASE FUNCTION; MODEL; CALIBRATION; EVOLUTION; INVERSION; ALBEDOS; CURVES; SHAPE;
D O I
10.1051/0004-6361/202245304
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Infrared measurements of asteroids are crucial for the determination of physical and thermal properties of individual objects, and for understanding the small-body populations in the solar system as a whole. However, standard radiometric methods can only be applied if the orbit of an object is known, hence its position at the time of the observation. With JWST-MIRI observations the situation will change and many unknown, often very small, solar system objects will be detected. Later orbit determinations are difficult due to the faintness of the objects and the lack of dedicated follow-up concepts. We present MIRI observations of the outer-belt asteroid (10920) 1998 BC1 and an unknown object, detected in all nine MIRI bands in close apparent proximity to (10920). We developed a new method called STM-ORBIT to interpret the multi-band measurements without knowing the object's true location. The power of the new technique is that it determines the most-likely heliocentric and observer-centric distance and phase angle ranges, allowing us to make a radiometric size estimate. The application to the MIRI fluxes of (10920) was used to validate the method. It leads to a confirmation of the known radiometric size-albedo solution, and puts constraints on the asteroid's location and orbit in agreement with its true orbit. To back up the validation of the method, we obtained additional ground-based light curve observations of (10920), combined with Gaia data, which indicate a very elongated object (a/b >= 1.5), with a spin-pole at (lambda, beta)(ecl)= (178(?), +81(?)), with an estimated error of about 20(?), and a rotation period of 4.861191 +/- 0.000015 h. A thermophysical study of all available JWST-MIRI and WISE measurements leads to a size of 14.5-16.5 km (diameter of an equal-volume sphere), a geometric albedo pV between 0.05 and 0.10, and a thermal inertia in the range 9-35 (best value 15) J m(-2) s-0.5 K-1. For the newly discovered MIRI object, the STM-ORBIT method revealed a size of 100-230 m. The new asteroid must be on a low-inclination orbit (0.7(?) < i < 2.0(?)) and it was located in the inner main-belt region during JWST observations. A beaming parameter eta larger than 1.0 would push the size even below 100 meters, a main-belt regime that has escaped IR detections so far. This kind of MIRI observations can therefore contribute to formation and evolution studies via classical size-frequency studies, which are currently limited to objects larger than about one kilometer in size. We estimate that MIRI frames with pointings close to the ecliptic and short integration times of only a few seconds will always include a few asteroids; most of them will be unknown objects.
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页数:16
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