325 Heidelberga
| Discovery | |
|---|---|
| Discovered by | Max Wolf |
| Discovery date | 4 March 1892 |
| Designations | |
Named after | Heidelberg |
| Main belt | |
| Orbital characteristics[1] | |
| Epoch 31 July 2016 (JD 2457600.5) | |
| Uncertainty parameter 0 | |
| Observation arc | 117.86 yr (43050 d) |
| Aphelion | 3.7223 AU (556.85 Gm) |
| Perihelion | 2.69998 AU (403.911 Gm) |
| 3.21115 AU (480.381 Gm) | |
| Eccentricity | 0.15919 |
| 5.75 yr (2101.8 d) | |
Average orbital speed | 16.64 km/s |
| 7.2090° | |
| 0° 10m 16.608s / day | |
| Inclination | 8.5545° |
| 344.881° | |
| 68.563° | |
| Earth MOID | 1.72396 AU (257.901 Gm) |
| Jupiter MOID | 1.78436 AU (266.936 Gm) |
| Jupiter Tisserand parameter | 3.154 |
| Physical characteristics | |
| Dimensions | 75.72±1.7 km |
| 6.737 h (0.2807 d) | |
| 0.1068±0.005 | |
| 8.65 | |
|
| |
325 Heidelberga is a large Main belt asteroid that was discovered by German astronomer Max Wolf on March 4, 1892 in Heidelberg.
Based upon its spectrum, 325 Heidelberga is classified as an M-type asteroid. No absorption features have been detected with certainty, indicating it most likely has a nickel-iron or enstatite chondrite composition.[2]
References
- ↑ Yeomans, Donald K., "325 Heidelberga", JPL Small-Body Database Browser, NASA Jet Propulsion Laboratory, retrieved 11 May 2016.
- ↑ Hardersen, Paul S.; Gaffey, Michael J.; Abell, Paul A. (January 1983), "Near-IR spectral evidence for the presence of iron-poor orthopyroxenes on the surfaces of six M-type asteroids" (PDF), Icarus, 175 (1), pp. 141–158, Bibcode:2005Icar..175..141H, doi:10.1016/j.icarus.2004.10.017, retrieved 2013-03-30.
External links
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