41 Daphne is a largeasteroid from theasteroid belt.[1] It is a dark-surfaced body 174 km in diameter is probably composed of primitivecarbonaceouschondrites. The spectra of the asteroid displays evidence of aqueous alteration.[8] It was discovered byH. Goldschmidt on May 22, 1856, and named afterDaphne, thenymph inGreek mythology who was turned into alaurel tree. Incorrect orbital calculations initially resulted in56 Melete being mistaken for a second sighting of Daphne. Daphne was not sighted again until August 31, 1862.[9]
The orbit of 41 Daphne places it in a 9:22mean motion resonance with the planetMars. The computedLyapunov time for this asteroid is 14,000 years, indicating that it occupies a chaotic orbit that will change randomly over time because ofgravitational perturbations of the planets.[10]
In 1999, Daphneocculted threestars, and on July 2, 1999, produced elevenchords indicating an ellipsoid of 213×160 km.[4] Daphneanlightcurves also suggest that the asteroid is irregular in shape. Daphne was observed byAreciboradar in April 2008.[11][12] Based upon radar data, the near surface solid density of the asteroid is 2.4+0.7 −0.5 g cm−3.[13]
41 Daphne has at least one satellite, namedPeneius (provisionallyS/2008 (41) 1).[14][15] It was identified on March 28, 2008, and has a projected separation of 443 km, an orbital period of approximately 1.1 days,[5] and an estimated diameter of less than 2 km. If these preliminary observations hold up, this binary system has the most extreme size ratio known.[16]In Greek myth,Pēneios is the god of theriver of that name, and father of Daphne.
^abcdeP. Vernazza et al. (2021) VLT/SPHERE imaging survey of the largest main-belt asteroids: Final results and synthesis.Astronomy & Astrophysics 54, A56
^Matter, Alexis; Marco Delbo; Sebastiano Ligori; Nicolas Crouzet; Paolo Tanga (2011). "Determination of physical properties of the asteroid (41) Daphne from interferometric observations in the thermal infrared".Icarus.215 (1):47–56.arXiv:1108.2616.Bibcode:2011Icar..215...47M.doi:10.1016/j.icarus.2011.07.012.
^Fornasier, S.; et al. (February 1999), "Spectroscopic comparison of aqueous altered asteroids with CM2 carbonaceous chondrite meteorites",Astronomy and Astrophysics Supplement,135: 65−73,Bibcode:1999A&AS..135...65F,doi:10.1051/aas:1999161.
^Šidlichovský, M. (1999), Svoren, J.; Pittich, E. M.; Rickman, H. (eds.), "Resonances and chaos in the asteroid belt",Evolution and source regions of asteroids and comets : proceedings of the 173rd colloquium of the International Astronomical Union, held in Tatranska Lomnica, Slovak Republic, August 24–28, 1998, pp. 297–308,Bibcode:1999esra.conf..297S.