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<!-- Additional parameters for this template  are available at [[Template:Infobox Planet]]. -->
{{Infobox planet
| discovery=yes
| physical_characteristics = yes
| bgcolour=#FFFFC0
| name=6 Hebe
| symbol= [[Image:6 Hebe Astronomical Symbol.svg|30px]]
| discoverer=[[Karl Ludwig Hencke]]
| discovered=July 1, 1847
| image=
| alt_names=1947 JB
| pronounced = {{IPAc-en|ˈ|h|iː|b|iː}} {{Respell|HEE|bee}}
| adjectives = Hebean
| named_after = [[Hebe (mythology)|Hēbē]]
| mp_category=[[Main belt]]
| epoch=November 26, 2005 ([[Julian day|JD]] 2453700.5)
| semimajor=2.426 AU (362.851 Gm)
| perihelion=1.937 AU (289.705 Gm)
| aphelion=2.914 [[Astronomical unit|AU]] (435.996 Gm)
| eccentricity=0.202
| period=3.78 [[Julian year (astronomy)|a]] (1379.756 d)
| inclination=14.751°
| asc_node=138.752°
| arg_peri=239.492°
| mean_anomaly=247.947°
| avg_speed=18.93 km/s
| p_orbit_ref = <ref name=Hebe-POE>{{cite web
  |title=AstDyS-2 Hebe Synthetic Proper Orbital Elements
  |publisher=Department of Mathematics, University of Pisa, Italy
  |url=http://hamilton.dm.unipi.it/astdys/index.php?pc=1.1.6&n=6
  |accessdate=2011-10-01}}</ref>
| p_semimajor = 2.4252710
| p_eccentricity = 0.1584864
| p_inclination = 14.3511092°
| p_mean_motion = 95.303184
| perihelion_rate = 31.568209
| node_rate = −41.829042
| dimensions=205×185×170 km<ref name=Baer/><ref name=IRAS>[http://www.psi.edu/pds/archive/astdata04/simps04/diamalb.tab Supplemental IRAS Minor Planet Survey]</ref><ref name=Torppa2003>[http://www.rni.helsinki.fi/~mjk/thirty.pdf J. Torppa et al. ''Shapes and rotational properties of thirty asteroids from photometric data''], Icarus, Vol. 164, p. 346 (2003).</ref><br>186 km ([[Geometric mean|mean]])
| mass=1.28{{e|19}} kg<ref name=Baer>{{Cite web
  |year=2008
  |title=Recent Asteroid Mass Determinations
  |publisher=Personal Website
  |author=Jim Baer
  |url=http://home.earthlink.net/~jimbaer1/astmass.txt
  |accessdate=2008-11-28}}</ref>
| density=3.81±0.26 g/cm³<ref name=Baer/>
| surface_grav=~0.087 m/s<sup>2</sup>
| escape_velocity=~0.13 km/s
| rotation=0.3031 d<ref>[http://www.psi.edu/pds/archive/lc.html Planetary Data System Small Bodies Node, lightcurve parameters]</ref>
| spectral_type=[[S-type asteroid]]
| magnitude = 7.5<ref name="Pasachoff1983">{{Cite book| author=Donald H. Menzel and Jay M. Pasachoff | year=1983 | title=A Field Guide to the Stars and Planets | edition=2nd edition | publisher=Houghton Mifflin | pages=391 | location=Boston, MA | isbn=0-395-34835-8 }}</ref> to 11.50
| abs_magnitude=5.71
| albedo=0.268&nbsp;([[geometric albedo|geometric]])<ref name=IRAS />
| angular_size = 0.26" <!-- Horizons 2010-Sep-20 --> to 0.065"
| single_temperature=~170 [[kelvin|K]] <br>''max:'' ~269 K (-4°C)
}}
'''6 Hebe''' ({{IPAc-en|ˈ|h|iː|b|iː}} {{Respell|HEE|bee}}) is a large [[main-belt]] [[asteroid]], containing around half a percent of the mass of the belt. Its apparently high bulk density (greater than that of the Earth's [[Moon]] or even [[Mars]]), however, means that by volume it does not rank among the top twenty asteroids. This high bulk density suggests an extremely solid body that has not been impacted by collisions, which is not typical of asteroids of its size – they tend to be loosely bound [[rubble pile]]s.


In [[apparent magnitude|brightness]], Hebe is the fifth brightest object in the asteroid belt after [[4 Vesta|Vesta]], [[Ceres (dwarf planet)|Ceres]], [[7 Iris|Iris]] and [[2 Pallas|Pallas]]. It has a mean opposition magnitude of +8.3, about equal to the mean brightness of [[Titan (moon)|Titan]]<ref>[http://jas.org.jo/ast.html The Brightest Asteroids]</ref> and can reach +7.5 at an opposition near perihelion.


Hebe is probably the parent body of the [[H chondrite]] meteorites, which account for a remarkable 40% of all [[meteorite]]s striking the Earth.
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==Discovery==
[[Image:Moon and Asteroids 1 to 10.svg|thumb|left|Size comparison: the first 10 asteroids profiled against Earth's [[Moon]]. Hebe is sixth from the left.]]
Hebe was the sixth [[asteroid]] to be discovered, on July 1, 1847 by [[Karl Ludwig Hencke]]. It was the second and final asteroid discovery by Hencke, who had previously found [[5 Astraea]]. The name ''[[Hebe (mythology)|Hebe]]'', goddess of youth, was proposed by [[Carl Friedrich Gauss]].
 
==Major meteorite source==
'''6 Hebe''' is the probable parent body of the [[H chondrite]] [[meteorite]]s and the [[IIE iron meteorite]]s.
[[Image:HebeOrbit.png|left|thumb|270px|The orbit of 6 Hebe compared with the orbits of Earth, Mars and Jupiter]]
Remarkably, this would imply that it is the source of about 40% of all meteorites striking the Earth. Evidence for this connection includes the following (after Michael Gaffey and Sarah L. Gilbert.<ref name=GaffeyGilbert>[http://adsabs.harvard.edu/cgi-bin/nph-bib_query?bibcode=1998M%26PS...33.1281G&amp;db_key=AST&amp;data_type=HTML&amp;format=&amp;high=438c93072f28336 M. J. Gaffey & S. L. Gilbert ''Asteroid 6 Hebe: The probable parent body of the H-Type ordinary chondrites and the IIE iron meteorites''], Meteoritics & Planetary Science, Vol. 33, p. 1281 (1998).</ref>):
* The spectrum of Hebe matches a mix of 60% H chondrite and 40% IIE iron meteorite material.
* The IIE type are unusual among the iron meteorites, and probably formed from impact melt, rather than being fragments of the core of a [[planetary differentiation|differentiated]] asteroid.
* The IIE irons and H chondrites likely come from the same parent body, due to similar trace mineral and oxygen [[isotope]] ratios.
* Asteroids with spectra similar to the [[ordinary chondrite]] meteorites (accounting for 85% of all falls, including the H chondrites) are extremely rare.
* 6 Hebe is extremely well placed to send impact debris to Earth-crossing orbits. Ejecta with even relatively small velocities (~280&nbsp;m/s) can enter the chaotic regions of the 3:1 [[Kirkwood gap]] at 2.50 [[astronomical unit|AU]] and the nearby <math>\nu_6\,\!</math> [[secular resonance]] which determines the high-inclination edge of the [[asteroid belt]] at about 16°  [[inclinations]] hereabouts.
* Of the asteroids in this "well-placed" orbit, Hebe is the largest.
* An analysis of likely contributors to the Earth's meteorite flux places 6 Hebe at the top of the list,<ref name=Morbidelli1994>[http://articles.adsabs.harvard.edu/cgi-bin/nph-iarticle_query?1994A%26A...282..955M&amp;data_type=PDF_HIGH&amp;type=PRINTER&amp;filetype=.pdf A. Morbidelli et al. ''Delivery of meteorites through the &nu;<sub>6</sub> secular resonance''], Astronomy & Astrophysics, Vol. 282, p. 955 (1994).</ref> due to its position and relatively large size. ''If Hebe is not the H-chondrite parent body, then where are the meteorites from Hebe?''<ref name=GaffeyGilbert />
 
==Physical characteristics==
Lightcurve analysis suggests that Hebe has a rather angular shape, which may be due to several large impact craters.<ref name=Torppa2003 /> Hebe rotates in a [[prograde and retrograde motion|prograde]] direction, with the north pole pointing towards [[ecliptic coordinate system|ecliptic coordinates]] (β, λ) = (45°, 339°)  with a 10° uncertainty.<ref name=Torppa2003 /> This gives an [[axial tilt]] of 42°.
 
It has a bright surface and, if its identification as the parent body of the H chondrites is correct, a
surface composition of [[silicate]] [[chondritic]] rocks mixed with pieces of [[nickel]]-[[iron]] [[metal]]. A likely scenario for the formation of the surface metal is as follows:
# Large impacts caused local melting of the iron rich H chondrite surface. The metals, being heavier, would have settled to the bottom of the magma lake, forming a metallic layer buried by a relatively shallow layer of silicates.
# Later sizeable impacts broke up and mixed these layers.
# Small frequent impacts tend to preferentially pulverize the weaker rocky debris, leading to an increased concentration of the larger metal fragments at the surface, such that they eventually comprise ~40% of the immediate surface at the present time.
 
==Moon==
On March 5, 1977 Hebe [[occultation|occulted]] Kaffaljidhma ([[Gamma Ceti|γ Ceti]]), a moderately bright 3rd [[apparent magnitude|magnitude]] [[star]]. No other observed occultations by Hebe have been reported.
 
As a result of that occultation, a small Hebean [[natural satellite|moon]] was reported by [[Paul D. Maley]].<ref>[http://www.johnstonsarchive.net/astro/asteroidmoonsq.html W. R. Johnston ''Other reports of Asteroid/TNO Companions]</ref> It was nicknamed "Jebe" (see [[Heebie-jeebies (idiom)|Heebie Jeebies]]). This is the first modern day suggestion that asteroids have satellites. It was 17 years later when the first asteroid moon was formally discovered (Dactyl, the satellite of Ida.) However, the discovery of Hebe's moon has not been confirmed.
 
{{Clear}}
 
==References==
<references/>
 
==External links==
* [http://www.rni.helsinki.fi/~mjk/thirty.pdf shape model deduced from lightcurve]
* [http://adsabs.harvard.edu//full/seri/MNRAS/0007//0000283.000.html MNRAS '''7''' (1847) 283] (discovery announcement)
* [http://adsabs.harvard.edu//full/seri/MNRAS/0008//0000104.000.html MNRAS '''8''' (1848) 103]
* [http://ssd.jpl.nasa.gov/horizons.cgi?find_body=1&body_group=sb&sstr=6 JPL Ephemeris]
 
{{MinorPlanets Navigator|5 Astraea|7 Iris}}
{{MinorPlanets_Footer}}
 
{{DEFAULTSORT:Hebe}}
[[Category:Main Belt asteroids]]
[[Category:Asteroids named from Greek mythology]]
[[Category:S-type asteroids]]
[[Category:Astronomical objects discovered in 1847]]

Latest revision as of 12:00, 9 December 2014


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