6 Hebe

History

Hebe was discovered on 1 July 1847 by German astronomer Karl Ludwig Hencke in the town of Driesen, Brandenburg, Prussia (now Drezdenko, Poland). It is the sixth asteroid discovered. It was the second and final asteroid discovery by Hencke, after 5 Astraea. The name Hebe, after the Greek goddess of youth, was proposed by Carl Friedrich Gauss at Hencke's request. The first asteroids discovered had widely been considered planets by astronomers, but the rapid discoveries of several new asteroids in the late 1840s complicated the classification of asteroids. In the years following its discovery, Hebe was variously labelled as a planet, small planet, or asteroid. Eventually, throughout the latter half of the 19th century, the terms "asteroid" and "minor planet" became favored, although some astronomers continued referring to Hebe as a planet in this period.

Gauss chose a wineglass as Hebe's astronomical symbol. It was encoded in Unicode 17.0 as U+1CEC0 𜻀 ([[File:Hebe symbol (fixed width).svg|12px|class=skin-invert]]).{{cite web | access-date = September 9, 2025

On 5 March 1977, Hebe occulted the star γ Ceti A (Kaffaljidhma).

Orbit

Hebe orbits the Sun with an average distance (or semi-major axis) of 2.426 astronomical units (AU), placing it in the inner section of the main asteroid belt. Its distance to the Sun varies from 1.935 AU at perihelion to 2.917 AU at aphelion due to its moderately elliptical orbit, indicated by its orbital eccentricity of 0.202. It has an orbital period of 3.778 Earth years, following an orbit inclined by 14.74° with respect to the ecliptic plane.

Hebe resides near but does not participate in several orbital resonances. It orbits close to the 3:1 mean-motion resonance (MMR) with Jupiter at approximately 2.50 AU. Asteroids caught in the 3:1 Jovian MMR have orbital periods one-third that of Jupiter's; their orbits are destabilized and they are eventually removed by encounters with the planets, creating the 3:1 Kirkwood gap. Hebe is also located near the destabilizing \nu_{\rm 6} (g = g_{\rm 6}) secular resonance with Saturn, which at Hebe's average distance of 2.426 AU is located at 15–16° inclination.

Possible Hebe family

In the 1990s, Hebe was identified as a possible source for H chondrites and IIE iron meteorites. Its location near the 3:1 Jovian MMR and the \nu_{\rm 6} Saturnian secular resonance means that fragments created by impact events are easily destabilized into Earth-crossing orbits, where they could eventually impact Earth as meteorites. Indeed, the H chondritic surface compositions of two near-Earth objects(4953) 1990 MU and 2007 LEpoint towards Hebe as their parent body. Spectral observations of asteroids near the 3:1 Kirkwood gap in the early 2010s identified 695 Bella, 1166 Sakuntala, and 1607 Mavis as potential relatives of Hebe. However, they are located on the opposite side of the 3:1 Kirkwood gap, indicating that they jumped across the gap. In 2020, a study led by Sherry K. Fieber-Beyer identified nine additional candidate members of the tentative Hebe family, with some located on Hebe's side of the 3:1 Kirkwood gap.

Physical characteristics

Hebe is a large asteroid, with a volume-equivalent spheroidal diameter of 193 ±. Though Hebe's shape approximates an oblate spheroid, it hosts numerous extreme topographical features. Five large depressions have been identified on its surface, possibly representing deep impact craters. The depressions range from around 50 km to over 100 km in size, with depths between 7 and. Hebe additionally has a large, flattened face, giving it the appearance of a "lopped-off tooth". This large facet may represent a section of the asteroid that was blasted away into space by an ancient impact event.

Based on Hebe's lightcurve, or variations in its observed brightness, it rotates in a prograde (counterclockwise) direction with a rotation period of 7.27 hours. Its north pole pointing towards ecliptic coordinates (β, λ) = (45°, 339°) with a 10° uncertainty.

Spectrum and composition

Hebe is classified as an S-type asteroid under the Tholen classification scheme. Planetary scientist Michael James Gaffey further subdivided S-type asteroids into seven mineralogical subclasses, categorizing Hebe as an S(IV)-type asteroid. Hebe's S(IV) classification indicates its surface is silicate (or stony) in composition and undifferentiated or partially differentiated.

Notes

References

References

1. Noah Webster (1884) ''A Practical Dictionary of the English Language''
2. Gabriel Nisbet (1733) ''Caledon's Tears''
3. [http://www.psi.edu/pds/archive/astdata04/simps04/diamalb.tab Supplemental IRAS Minor Planet Survey] {{webarchive. link. (23 June 2006)
4. Donald H. Menzel. (1983). "A Field Guide to the Stars and Planets". Houghton Mifflin.
5. [http://jas.org.jo/ast.html The Brightest Asteroids] {{webarchive. link. (2008-05-11)
6. (18 September 2023). "Unicode request for historical asteroid symbols". Unicode.
7. "Not the mother of meteorites".
8. (December 1977). "Possible Observation of a Satellite of a Minor Planet". [[The Minor Planet Bulletin]].