Discovery [1] | |
---|---|
Discovered by | O. Oikawa |
Discovery site | Tokyo Obs. ( 389) |
Discovery date | 23 January 1927 |
Designations | |
(1266) Tone | |
Pronunciation |
/ˈtoʊni/ Japanese: [tone] |
Named after |
Tone River
[2] (Japanese river) |
1927 BD · 1933 BM 1934 EC · A899 PH | |
main-belt · (
outer)
[1]
[3] background [4] | |
Orbital characteristics [1] | |
Epoch 4 September 2017 ( JD 2458000.5) | |
Uncertainty parameter 0 | |
Observation arc | 84.76 yr (30,958 days) |
Aphelion | 3.5313 AU |
Perihelion | 3.1886 AU |
3.3600 AU | |
Eccentricity | 0.0510 |
6.16 yr (2,250 days) | |
102.82 ° | |
0° 9m 36s / day | |
Inclination | 17.182° |
320.63° | |
298.20° | |
Physical characteristics | |
Dimensions | 70.70±24.76 km
[5] 73.34±3.8 km [6] 75.470±0.523 km [7] 83.261±2.040 km [8] 88.82±1.33 km [9] 94.10±24.67 km [10] |
7.40±0.05
h
[11]
[a] 11.82±0.05 h [12] 12.9±0.1 h [13] | |
0.039±0.001
[9] 0.0439±0.0101 [8] 0.05±0.03 [10] 0.05±0.04 [5] 0.053±0.005 [7] 0.0566±0.006 [6] | |
Tholen = P
[1]
[3] B–V = 0.732 [1] U–B = 0.317 [1] | |
9.40 [10] · 9.41 [1] [3] [5] [6] [8] [9] | |
1266 Tone /ˈtoʊni/ is a dark background asteroid from the outer regions of the asteroid belt, approximately 80 kilometers in diameter. Discovered by astronomer Okuro Oikawa at the Tokyo Observatory in 1927, [14] it was assigned the provisional designation 1927 BD. The asteroid was later named after the Tone River, one of Japan's largest rivers. [2]
It was discovered by Japanese astronomer Okuro Oikawa at the Tokyo Observatory ( 389) on 23 January 1927. [14] On the following night, it was independently discovered by Soviet astronomer Grigory Neujmin at the Simeiz Observatory on the Crimean peninsula. [2] The Minor Planet Center only recognizes the first discoverer. [14] In August 1899, the asteroid was first identified as A899 PH at the Boyden Station of the Harvard Observatory in Arequipa, Peru. [14]
Tone is a non- family asteroid from the main belt's background population. [4] It orbits the Sun in the outer asteroid belt at a distance of 3.2–3.5 AU once every 6 years and 2 months (2,250 days; semi-major axis of 3.36 AU). Its orbit has an eccentricity of 0.05 and an inclination of 17 ° with respect to the ecliptic. [1]
The body's observation arc begins with its identification as 1933 BM at the German Heidelberg Observatory in January 1933, or four years after its official discovery observation at Tokyo. [14]
In the Tholen classification, Tone is a primitive and dark P-type asteroid. [1] [3]
In October 1999, two rotational lightcurves of Tone were obtained from photometric observations by American astronomer Brian Warner at his Palmer Divide Observatory ( 716) in Colorado. Lightcurve analysis gave two divergent rotation periods of 7.40 and 11.82 hours with a brightness variation of 0.06 and 0.12 magnitude, respectively ( U=2/2). [11] [12] [a] Observation by Italian astronomers Roberto Crippa and Federico Manzini in October 2005, gave another tentative period of 12.9 hours and an amplitude of 0.07 magnitude ( U=2-). [13] The LCDB currently adopts a period of 7.40 hours. [3]
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, Tone measures between 70.70 and 94.10 kilometers in diameter and its surface has an albedo between 0.039 and 0.0566. [5] [6] [7] [8] [9] [10]
The Collaborative Asteroid Lightcurve Link adopts the results obtained by IRAS, that is, an albedo of 0.0566 and a diameter of 73.34 kilometers based on an absolute magnitude of 9.41. [3]
This minor planet was named after Tone River (Tone-gawa), Japan's second-largest river after the Shinano River. [2] The official naming citation was mentioned in The Names of the Minor Planets by Paul Herget in 1955 ( H 116).
Discovery [1] | |
---|---|
Discovered by | O. Oikawa |
Discovery site | Tokyo Obs. ( 389) |
Discovery date | 23 January 1927 |
Designations | |
(1266) Tone | |
Pronunciation |
/ˈtoʊni/ Japanese: [tone] |
Named after |
Tone River
[2] (Japanese river) |
1927 BD · 1933 BM 1934 EC · A899 PH | |
main-belt · (
outer)
[1]
[3] background [4] | |
Orbital characteristics [1] | |
Epoch 4 September 2017 ( JD 2458000.5) | |
Uncertainty parameter 0 | |
Observation arc | 84.76 yr (30,958 days) |
Aphelion | 3.5313 AU |
Perihelion | 3.1886 AU |
3.3600 AU | |
Eccentricity | 0.0510 |
6.16 yr (2,250 days) | |
102.82 ° | |
0° 9m 36s / day | |
Inclination | 17.182° |
320.63° | |
298.20° | |
Physical characteristics | |
Dimensions | 70.70±24.76 km
[5] 73.34±3.8 km [6] 75.470±0.523 km [7] 83.261±2.040 km [8] 88.82±1.33 km [9] 94.10±24.67 km [10] |
7.40±0.05
h
[11]
[a] 11.82±0.05 h [12] 12.9±0.1 h [13] | |
0.039±0.001
[9] 0.0439±0.0101 [8] 0.05±0.03 [10] 0.05±0.04 [5] 0.053±0.005 [7] 0.0566±0.006 [6] | |
Tholen = P
[1]
[3] B–V = 0.732 [1] U–B = 0.317 [1] | |
9.40 [10] · 9.41 [1] [3] [5] [6] [8] [9] | |
1266 Tone /ˈtoʊni/ is a dark background asteroid from the outer regions of the asteroid belt, approximately 80 kilometers in diameter. Discovered by astronomer Okuro Oikawa at the Tokyo Observatory in 1927, [14] it was assigned the provisional designation 1927 BD. The asteroid was later named after the Tone River, one of Japan's largest rivers. [2]
It was discovered by Japanese astronomer Okuro Oikawa at the Tokyo Observatory ( 389) on 23 January 1927. [14] On the following night, it was independently discovered by Soviet astronomer Grigory Neujmin at the Simeiz Observatory on the Crimean peninsula. [2] The Minor Planet Center only recognizes the first discoverer. [14] In August 1899, the asteroid was first identified as A899 PH at the Boyden Station of the Harvard Observatory in Arequipa, Peru. [14]
Tone is a non- family asteroid from the main belt's background population. [4] It orbits the Sun in the outer asteroid belt at a distance of 3.2–3.5 AU once every 6 years and 2 months (2,250 days; semi-major axis of 3.36 AU). Its orbit has an eccentricity of 0.05 and an inclination of 17 ° with respect to the ecliptic. [1]
The body's observation arc begins with its identification as 1933 BM at the German Heidelberg Observatory in January 1933, or four years after its official discovery observation at Tokyo. [14]
In the Tholen classification, Tone is a primitive and dark P-type asteroid. [1] [3]
In October 1999, two rotational lightcurves of Tone were obtained from photometric observations by American astronomer Brian Warner at his Palmer Divide Observatory ( 716) in Colorado. Lightcurve analysis gave two divergent rotation periods of 7.40 and 11.82 hours with a brightness variation of 0.06 and 0.12 magnitude, respectively ( U=2/2). [11] [12] [a] Observation by Italian astronomers Roberto Crippa and Federico Manzini in October 2005, gave another tentative period of 12.9 hours and an amplitude of 0.07 magnitude ( U=2-). [13] The LCDB currently adopts a period of 7.40 hours. [3]
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, Tone measures between 70.70 and 94.10 kilometers in diameter and its surface has an albedo between 0.039 and 0.0566. [5] [6] [7] [8] [9] [10]
The Collaborative Asteroid Lightcurve Link adopts the results obtained by IRAS, that is, an albedo of 0.0566 and a diameter of 73.34 kilometers based on an absolute magnitude of 9.41. [3]
This minor planet was named after Tone River (Tone-gawa), Japan's second-largest river after the Shinano River. [2] The official naming citation was mentioned in The Names of the Minor Planets by Paul Herget in 1955 ( H 116).