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382 Dodona

From Wikipedia, the free encyclopedia
Main-belt asteroid

382 Dodona
A three-dimensional model of 382 Dodona based on its light curve
Discovery
Discovered byAuguste Charlois
Discovery date29 January 1894
Designations
(382) Dodona
Pronunciation/dəˈdnə/[1]
Named after
Dodona
1894 AT
Main belt
Orbital characteristics[2]
Epoch 31 July 2016 (JD 2457600.5)
Uncertainty parameter 0
Observation arc122.21 yr (44636 d)
Aphelion3.6577 AU (547.18 Gm)
Perihelion2.58301 AU (386.413 Gm)
3.1204 AU (466.81 Gm)
Eccentricity0.17221
5.51yr (2013.3d)
6.32892°
0° 10m 43.716s / day
Inclination7.3928°
313.511°
270.036°
Physical characteristics
Dimensions58.37±2.8 km[2]
58.37 km[3]
4.113 h (0.1714 d)
0.1610±0.017[2]
0.161[3]
M
8.77[2][3]

382 Dodona is a largeMain beltasteroid that was discovered by the French astronomerAuguste Charlois on 29 January 1894 inNice. It is classified as anM-type asteroid.

Measurements of thethermal inertia of 115 Thyra give an estimated range of 15–150 J m−2 K−1 s−1/2, compared to 50 forlunar regolith and 400 for coarse sand in an atmosphere.[3]

References

[edit]
  1. ^"Dodona".Dictionary.com Unabridged (Online). n.d.
  2. ^abcd"382 Dodona (1894 AT)".JPL Small-Body Database.NASA/Jet Propulsion Laboratory. Retrieved10 May 2016.
  3. ^abcdDelbo', Marco; Tanga, Paolo (February 2009), "Thermal inertia of main belt asteroids smaller than 100 km from IRAS data",Planetary and Space Science, vol. 57, no. 2, pp. 259–265,arXiv:0808.0869,Bibcode:2009P&SS...57..259D,doi:10.1016/j.pss.2008.06.015.

External links

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