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1390 Abastumani

Large main-belt asteroid


Large main-belt asteroid

FieldValue
minorplanetyes
name1390 Abastumani
background#D6D6D6
image001390-asteroid shape model (1390) Abastumani.png
captionShape model of *Abastumani* from its lightcurve
discovery_ref
discovered3 October 1935
discovererP. Shajn
discovery_siteSimeiz Obs.
mpc_name(1390) Abastumani
alt_names1935 TA1926 GN
1929 ULA907 GN
A916 VA
named_afterAbastumani
(Georgian town)
mp_category{{plainlist
* main-belt<ref name"MPC-object" /(outer)
* background<ref name"AstDys-object" /}}
orbit_ref
epoch16 February 2017 (JD 2457800.5)
uncertainty0
observation_arc86.80 yr (31,705 days)
aphelion3.5547 AU
perihelion3.3166 AU
semimajor3.4356 AU
eccentricity0.0347
period6.37 yr (2,326 days)
mean_anomaly290.65°
mean_motion/ day
inclination19.932°
asc_node28.919°
arg_peri332.76°
mean_diameter
km
km (IRAS:12)
km
rotation
albedo
(IRAS:12)
spectral_type{{plainlist
* Tholen {{}} P
* B–V {{}} 0.685
* U–B {{}} 0.189
abs_magnitude9.40

1929 ULA907 GN A916 VA (Georgian town)

  • main-belt(outer)

  • background}} km km (IRAS:12) km (IRAS:12)

  • Tholen P

  • B–V 0.685

  • U–B 0.189

1390 Abastumani (prov. designation: ) is a very large and dark background asteroid from the outer region of the asteroid belt. It was discovered on 3 October 1935, by Russian astronomer Pelageya Shajn at the Simeiz Observatory on the Crimean peninsula. The primitive P-type asteroid has a rotation period of 17.1 hours and measures approximately 101 km in diameter. It was named for the Georgian town of Abastumani.

Orbit and classification

The dark and reddish asteroid is classified as a rare P-type asteroid in the Tholen taxonomic scheme, of which only a few dozens bodies are currently known. It orbits the Sun at a distance of 3.3–3.6 AU once every 6 years and 4 months (2,326 days). Its orbit has an eccentricity of 0.03 and an inclination of 20° with respect to the ecliptic. The first used precovery was taken at Lowell Observatory in 1929, extending the asteroid's observation arc by 6 years prior to its discovery.

Discovery

Abastumani was discovered on 3 October 1935, by Soviet–Russian astronomer Pelageya Shajn at Simeiz Observatory on the Crimean peninsula. On the same night, the asteroid was independently discovered by South African astronomer Cyril Jackson at Johannesburg Observatory. It was one of the last large-sized bodies discovered in the outer belt (also see 1269 Rollandia and 1902 Shaposhnikov, discovered in 1930 and 1972, respectively).

Naming

This minor planet is named after the spa town of Abastumani located in the Caucasus Mountains of Georgia. It is now the place where the Abastuman Astronomical Observatory is situated. The official was published by the Minor Planet Center in November 1952 (M.P.C. 838).

Physical characteristics

In the Tholen classification, Abastumani is a primitive, carbonaceous P-type asteroid, a common spectral type in the outer main-belt and among the Jupiter trojan population.

Rotation period

In April 2002, a rotational lightcurve of Abastumani was obtained from photometric observation by astronomer John Gross at the U.S. Sonoran Skies Observatory in Benson, Arizona. It gave a rotation period of hours with a brightness variation of 0.15 in magnitude ().

Diameter and albedo

According to the surveys carried out by the Infrared Astronomical Satellite IRAS, the Japanese Akari satellite, and the NEOWISE mission of NASA's Wide-field Infrared Survey Explorer, the asteroid measures between 98.3 and 107.8 kilometers in diameter, and its surface has a very low albedo between 0.026 and 0.033. The Collaborative Asteroid Lightcurve Link adopts the results obtained by IRAS, i.e. a diameter of 101.5 kilometers and an albedo of 0.0298.

References

Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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