382 Dodona
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A three-dimensional model of 382 Dodona based on its light curve. | |
| Discovery | |
|---|---|
| Discovered by | Auguste Charlois |
| Discovery date | January 29, 1894 |
| Designations | |
Named after | Dodona |
| 1894 AT | |
| Main belt | |
| Orbital characteristics | |
| Epoch 30 January 2005 (JD 2453400.5) | |
| Aphelion | 549.43 Gm (3.673 AU) |
| Perihelion | 383.503 Gm (2.564 AU) |
| 466.466 Gm (3.118 AU) | |
| Eccentricity | 0.178 |
| 2011.093 d (5.51 a) | |
Average orbital speed | 16.87 km/s |
| 333.617° | |
| Inclination | 7.403° |
| 313.654° | |
| 270.828° | |
| Physical characteristics | |
| Dimensions | 58.37[1] km |
| Albedo | 0.161[1] |
Spectral type | M |
| 8.77[1] | |
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382 Dodona is a large Main belt asteroid that was discovered by the French astronomer Auguste Charlois on January 29, 1894 in Nice. It is classified as an M-type asteroid.
Measurements of the thermal inertia of 115 Thyra give an estimated range of 15–150 J m−2 K−1 s−1/2, compared to 50 for lunar regolith and 400 for coarse sand in an atmosphere.[1]
References
- ↑ 1.0 1.1 1.2 1.3 Delbo', Marco; Tanga, Paolo (February 2009), "Thermal inertia of main belt asteroids smaller than 100 km from IRAS data", Planetary and Space Science 57 (2): 259–265, arXiv:0808.0869, Bibcode:2009P&SS...57..259D, doi:10.1016/j.pss.2008.06.015.
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