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Jupiter trojan

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Theasteroidsof theinner Solar SystemandJupiter
Jupiter trojans
Hilda asteroids
Asteroid belt
Orbitsofplanets
The Jupiter trojans are divided into two groups: TheGreek campin front of and theTrojan camptrailing behind Jupiter in their orbit.

TheJupiter trojans,commonly calledtrojan asteroidsor simplytrojans,are a large group ofasteroidsthat share the planetJupiter's orbit around theSun.Relative to Jupiter, eachtrojanlibratesaround one of Jupiter's stableLagrange points:eitherL4,existing 60° ahead of the planet in its orbit, orL5,60° behind. Jupiter trojans are distributed in two elongated, curved regions around these Lagrangian points with an averagesemi-major axisof about 5.2AU.[1]

The first Jupiter trojan discovered,588 Achilles,was spotted in 1906 by German astronomerMax Wolf.[2]More than 9,800 Jupiter trojans have been found as of May 2021.[3]By convention, they are each named fromGreek mythologyafter a figure of theTrojan War,hence the name "trojan". The total number of Jupiter trojans larger than 1 km in diameter is believed to be about1 million,[1]approximately equal to the number of asteroids larger than 1 km in theasteroid belt.[4]Like main-belt asteroids, Jupiter trojans formfamilies.[5]

As of 2004,many Jupiter trojans showed to observational instruments as dark bodies with reddish, featurelessspectra.No firm evidence of the presence of water, or any other specific compound on their surface has been obtained, but it is thought that they are coated intholins,organic polymers formed by the Sun's radiation.[6]The Jupiter trojans' densities (as measured by studyingbinariesor rotational lightcurves) vary from 0.8 to 2.5 g·cm−3.[5]Jupiter trojans are thought to have been captured into their orbits during the early stages of theSolar System's formationor slightly later, during themigrationof giant planets.[5]

The term "Trojan Asteroid" specifically refers to the asteroids co-orbital with Jupiter, but the general term "trojan"is sometimes more generally applied to othersmall Solar System bodieswith similar relationships to larger bodies:Mars trojans,Neptune trojans,Uranus trojansandEarth trojansare known to exist.[7][8][9]The term "Trojan asteroid" is normally understood to specifically mean the Jupiter trojans because the first Trojans were discovered near Jupiter's orbit and Jupiter currently has by far the most known Trojans.[3]

Observational history

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Maximilian Franz Joseph Cornelius Wolf(1890)—the discoverer of the first trojan

In 1772, Italian-born mathematicianJoseph-Louis Lagrange,in studying therestricted three-body problem,predicted that a small body sharing an orbit with a planet but lying 60° ahead or behind it will be trapped near these points.[2]The trapped body willlibrateslowly around the point of equilibrium in atadpoleorhorseshoe orbit.[10]These leading and trailing points are called the L4and L5Lagrange points.[11][Note 1]The first asteroids trapped in Lagrange points were observed more than a century after Lagrange's hypothesis. Those associated with Jupiter were the first to be discovered.[2]

E. E. Barnardmade the first recorded observation of a trojan,(12126) 1999 RM11(identified as A904 RD at the time), in 1904, but neither he nor others appreciated its significance at the time.[12]Barnard believed he had seen the recently discoveredSaturnian satellitePhoebe,which was only twoarc-minutesaway in the sky at the time, or possibly an asteroid. The object's identity was not understood until its orbit was calculated in 1999.[12]

The first accepted discovery of a trojan occurred in February 1906, when astronomerMax WolfofHeidelberg-Königstuhl State Observatorydiscovered anasteroidat the L4Lagrangian pointof theSunJupitersystem, later named588 Achilles.[2]In 1906–1907 two more Jupiter trojans were found by fellow German astronomerAugust Kopff(624 Hektorand617 Patroclus).[2]Hektor, like Achilles, belonged to the L4swarm ( "ahead" of the planet in its orbit), whereas Patroclus was the first asteroid known to reside at the L5Lagrangian point ( "behind" the planet).[13]By 1938, 11 Jupiter trojans had been detected.[14]This number increased to 14 only in 1961.[2]As instruments improved, the rate of discovery grew rapidly: by January 2000, a total of 257 had been discovered;[11]by May 2003, the number had grown to 1,600.[15]As of October 2018there are 4,601 known Jupiter trojans at L4and 2,439 at L5.[16]

Nomenclature

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The custom of naming all asteroids in Jupiter's L4and L5points after famous heroes of theTrojan Warwas suggested byJohann PalisaofVienna,who was the first to accurately calculate their orbits.[2]

Asteroids in the leading (L4) orbit are named afterGreekheroes (the "Greek node or camp" or "Achillesgroup "), and those at the trailing (L5) orbit are named after the heroes ofTroy(the "Trojan node or camp" ).[2]The asteroids617 Patroclusand624 Hektorwere named before the Greece/Troy rule was devised, resulting in a "Greek spy",Patroclus,in the Trojan node and a "Trojan spy",Hector,in the Greek node.[14][17]

In 2018, at its 30th General Assembly in Vienna, theInternational Astronomical Unionamended the naming convention for Jupiter trojans, allowing for asteroids withHlarger than 12 (that is, amean diametersmaller than approximately 22 kilometers, for an assumed albedo of 0.057) to be named after Olympic athletes, because there are now far more known Jupiter trojans than available names ofGreek and Trojan warriorsthat fought in the Trojan war.[18]

Numbers and mass

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Agravitational potentialcontour plot showing Earth's Lagrangian points; L4and L5are ahead (above) and behind (below) the planet, respectively. Jupiter's Lagrangian points are similarly situated in its much larger orbit.

Estimates of the total number of Jupiter trojans are based on deep surveys of limited areas of the sky.[1]The L4swarm is believed to hold between 160,000 and 240,000 asteroids with diameters larger than 2 km and about 600,000 with diameters larger than 1 km.[1][11]If the L5swarm contains a comparable number of objects, there are more than1 millionJupiter trojans 1 km in size or larger. For the objects brighter thanabsolute magnitude9.0 the population is probably complete.[15]These numbers are similar to that of comparable asteroids in the asteroid belt.[1]The total mass of the Jupiter trojans is estimated at 0.0001 of the mass of Earth or one-fifth of the mass of the asteroid belt.[11]

Two more recent studies indicate that the above numbers may overestimate the number of Jupiter trojans by several-fold. This overestimate is caused by (1) the assumption that all Jupiter trojans have a lowalbedoof about 0.04, whereas small bodies may have an average albedo as high as 0.12;[19](2) an incorrect assumption about the distribution of Jupiter trojans in the sky.[20]According to the new estimates, the total number of Jupiter trojans with a diameter larger than 2 km is6,300 ± 1,000and3,400 ± 500in the L4and L5swarms, respectively.[20]These numbers would be reduced by a factor of 2 if small Jupiter trojans are more reflective than large ones.[19]

The number of Jupiter trojans observed in the L4swarm is slightly larger than that observed in L5.Because the brightest Jupiter trojans show little variation in numbers between the two populations, this disparity is probably due to observational bias.[5]Some models indicate that the L4swarm may be slightly more stable than the L5swarm.[10]

The largest Jupiter trojan is624 Hektor,which has a mean diameter of 203 ± 3.6 km.[15]There are few large Jupiter trojans in comparison to the overall population. With decreasing size, the number of Jupiter trojans grows very quickly down to 84 km, much more so than in the asteroid belt. A diameter of 84 km corresponds to an absolute magnitude of 9.5, assuming analbedoof 0.04. Within the 4.4–40 km range the Jupiter trojans' size distribution resembles that of the main-belt asteroids. Nothing is known about the masses of the smaller Jupiter trojans.[10]The size distribution suggests that the smaller Trojans may be the products of collisions by larger Jupiter trojans.[5]

The largestJupiter trojans
Trojan Diameter (km)
624 Hektor 225
617 Patroclus 140
911 Agamemnon 131
588 Achilles 130
3451 Mentor 126
3317 Paris 119
1867 Deiphobus 118
1172 Äneas 118
1437 Diomedes 118
1143 Odysseus 115
Source:JPL Small-Body Database,NEOWISEdata

Orbits

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Animation of the orbit of 624 Hektor (blue), set against the orbit of Jupiter (outer red ellipse)

Jupiter trojans have orbits with radii between 5.05 and 5.35 AU (the mean semi-major axis is 5.2 ± 0.15 AU), and are distributed throughout elongated, curved regions around the two Lagrangian points;[1]each swarm stretches for about 26° along the orbit of Jupiter, amounting to a total distance of about 2.5 AU.[11]The width of the swarms approximately equals twoHill's radii,which in the case of Jupiter amounts to about 0.6 AU.[10]Many of Jupiter trojans have largeorbital inclinationsrelative to Jupiter's orbital plane—up to 40°.[11]

Jupiter trojans do not maintain a fixed separation from Jupiter. They slowly librate around their respective equilibrium points, periodically moving closer to Jupiter or farther from it.[10]Jupiter trojans generally follow paths calledtadpole orbitsaround the Lagrangian points; the average period of their libration is about 150 years.[11]The amplitude of the libration (along the Jovian orbit) varies from 0.6° to 88°, with the average being about 33°.[10]Simulations show that Jupiter trojans can follow even more complicated trajectories when moving from one Lagrangian point to another—these are calledhorseshoe orbits(currently no Jupiter Trojan with such an orbit is known, thoughoneis knownfor Neptune).[10]

Dynamical families and binaries

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Discerningdynamical familieswithin the Jupiter trojan population is more difficult than it is in the asteroid belt, because the Jupiter trojans are locked within a far narrower range of possible positions. This means that clusters tend to overlap and merge with the overall swarm. By 2003 roughly a dozen dynamical families were identified. Jupiter-trojan families are much smaller in size than families in the asteroid belt; the largest identified family, the Menelaus group, consists of only eight members.[5]

In 2001,617 Patrocluswas the first Jupiter trojan to be identified as abinary asteroid.[21]The binary's orbit is extremely close, at 650 km, compared to 35,000 km for the primary'sHill sphere.[22]The largest Jupiter trojan—624 Hektor— is probably acontact binarywith a moonlet.[5][23][24]

Physical properties

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Trojan624 Hektor(indicated) is similar inbrightnesstodwarf planetPluto.

Jupiter trojans are dark bodies of irregular shape. Theirgeometric albedosgenerally vary between 3 and 10%.[15]The average value is 0.056 ± 0.003 for the objects larger than 57 km,[5]and 0.121 ± 0.003 (R-band) for those smaller than 25 km.[19]The asteroid4709 Ennomoshas the highest albedo (0.18) of all known Jupiter trojans.[15]Little is known about the masses, chemical composition, rotation or other physical properties of the Jupiter trojans.[5]

Rotation

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The rotational properties of Jupiter trojans are not well known. Analysis of the rotationallight curvesof 72 Jupiter trojans gave an average rotational period of about 11.2 hours, whereas the average period of the control sample of asteroids in the asteroid belt was 10.6 hours.[25]The distribution of the rotational periods of Jupiter trojans appeared to be well approximated by aMaxwellian function,[Note 2]whereas the distribution for main-belt asteroids was found to be non-Maxwellian, with a deficit of periods in the range 8–10 hours.[25]The Maxwellian distribution of the rotational periods of Jupiter trojans may indicate that they have undergone a stronger collisional evolution compared to the asteroid belt.[25]

In 2008 a team fromCalvin Collegeexamined thelight curvesof a debiased sample of ten Jupiter trojans, and found amedianspin period of 18.9 hours. This value was significantly higher than that for main-belt asteroids of similar size (11.5 hours). The difference could mean that the Jupiter trojans possess a lower average density, which may imply that they formed in theKuiper belt(see below).[26]

Composition

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Spectroscopically,the Jupiter trojans mostly areD-type asteroids,which predominate in the outer regions of the asteroid belt.[5]A small number are classified asPorC-type asteroids.[25]Their spectra are red (meaning that they reflect more light at longer wavelengths) or neutral and featureless.[15]No firm evidence of water, organics or other chemical compounds has been obtained as of 2007.4709 Ennomoshas an albedo slightly higher than the Jupiter-trojan average, which may indicate the presence of water ice. Some other Jupiter Trojans, such as911 Agamemnonand617 Patroclus,have shown very weak absorptions at 1.7 and 2.3 μm, which might indicate the presence of organics.[27]The Jupiter trojans' spectra are similar to those of theirregular moons of Jupiterand, to a certain extent,comet nuclei,though Jupiter trojans are spectrally very different from the redder Kuiper belt objects.[1][5]A Jupiter trojan's spectrum can be matched to a mixture of water ice, a large amount of carbon-rich material (charcoal),[5]and possiblymagnesium-richsilicates.[25]The composition of the Jupiter trojan population appears to be markedly uniform, with little or no differentiation between the two swarms.[28]

A team from theKeck Observatoryin Hawaii announced in 2006 that it had measured the density of the binary Jupiter trojan617 Patroclusas being less than that of water ice (0.8 g/cm3), suggesting that the pair, and possibly many other Trojan objects, more closely resemblecometsor Kuiper belt objects in composition—water ice with a layer of dust—than they do the main-belt asteroids.[22]Countering this argument, the density of Hektor as determined from its rotational lightcurve (2.480 g/cm3) is significantly higher than that of 617 Patroclus.[24]Such a difference in densities suggests that density may not be a good indicator of asteroid origin.[24]

Origin and evolution

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Two main theories have emerged to explain the formation and evolution of the Jupiter trojans. The first suggests that the Jupiter trojans formed in the same part of theSolar Systemas Jupiter and entered their orbits while it was forming.[10]The last stage of Jupiter's formation involved runaway growth of its mass through the accretion of large amounts ofhydrogenandheliumfrom theprotoplanetary disk;during this growth, which lasted for only about 10,000 years, the mass of Jupiter increased by a factor of ten. Theplanetesimalsthat had approximately the same orbits as Jupiter were caught by the increased gravity of the planet.[10]The capture mechanism was very efficient—about 50% of all remaining planetesimals were trapped. This hypothesis has two major problems: the number of trapped bodies exceeds the observed population of Jupiter trojans by fourorders of magnitude,and the present Jupiter trojan asteroids have larger orbital inclinations than are predicted by the capture model.[10]Simulations of this scenario show that such a mode of formation also would inhibit the creation of similar trojans forSaturn,and this has been borne out by observation: to date no trojans have been found near Saturn.[29]In a variation of this theory Jupiter captures trojans during its initial growth then migrates as it continues to grow. During Jupiter's migration the orbits of objects in horseshoe orbits are distorted causing the L4 side of these orbits to be over occupied. As a result, an excess of trojans is trapped on the L4 side when the horseshoe orbits shift to tadpole orbits as Jupiter grows. This model also leaves the Jupiter trojan population 3–4 orders of magnitude too large.[30]

The second theory proposes that the Jupiter trojans were captured during the migration of the giant planets described in theNice model.In the Nice model the orbits of the giant planets became unstable500–600 millionyears after the Solar System's formation when Jupiter and Saturn crossed their 1:2 mean-motionresonance.Encounters between planets resulted inUranusandNeptunebeing scattered outward into the primordialKuiper belt,disrupting it and throwing millions of objects inward.[31]When Jupiter and Saturn were near their 1:2 resonance the orbits of pre-existing Jupiter trojans became unstable during a secondary resonance with Jupiter and Saturn. This occurred when the period of the trojans' libration about their Lagrangian point had a 3:1 ratio to the period at which the position where Jupiter passes Saturn circulated relative to its perihelion. This process was also reversible allowing a fraction of the numerous objects scattered inward by Uranus and Neptune to enter this region and be captured as Jupiter's and Saturn's orbits separated. These new trojans had a wide range of inclinations, the result of multiple encounters with the giant planets before being captured.[32]This process can also occur later when Jupiter and Saturn cross weaker resonances.[33]

In arevised versionof the Nice model Jupiter trojans are captured when Jupiter encounters an ice giant during the instability. In this version of the Nice model one of the ice giants (Uranus, Neptune, or a lostfifth planet) is scattered inward onto a Jupiter-crossing orbit and is scattered outward by Jupiter causing the orbits of Jupiter and Saturn to quickly separate. When Jupiter's semi-major axis jumps during these encounters existing Jupiter trojans can escape and new objects with semi-major axes similar to Jupiter's new semi-major axis are captured. Following its last encounter the ice giant can pass through one of the libration points and perturb their orbits leaving this libration point depleted relative to the other. After the encounters end some of these Jupiter trojans are lost and others captured when Jupiter and Saturn are near weak mean motion resonances such as the 3:7 resonance via the mechanism of the original Nice model.[33]

The long-term future of the Jupiter trojans is open to question, because multiple weak resonances with Jupiter and Saturn cause them to behave chaotically over time.[34]Collisional shattering slowly depletes the Jupiter trojan population as fragments are ejected. Ejected Jupiter trojans could become temporary satellites of Jupiter orJupiter-family comets.[5]Simulations show that the orbits of up to 17% of Jupiter trojans are unstable over the age of the Solar System.[35]Levison et al. believe that roughly 200 ejected Jupiter trojans greater than 1 km in diameter might be travelling the Solar System, with a few possibly on Earth-crossing orbits.[36]Some of the escaped Jupiter trojans may become Jupiter-family comets as they approach the Sun and their surface ice begins evaporating.[36]

Exploration

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On 4 January 2017 NASA announced thatLucywas selected as one of their next twoDiscovery Programmissions.[37]Lucyis set to explore seven[38]Jupiter trojans. It was launched on October 16, 2021, and will arrive at theL4Trojan cloud in 2027 after two Earth gravity assists and a fly-by of a main-belt asteroid. It will then return to the vicinity of Earth for another gravity assist to take it to Jupiter'sL5Trojan cloud where it will visit617 Patroclus.[39]

See also

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Notes

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  1. ^The three other points—L1,L2and L3—are unstable.[10]
  2. ^The Maxwellian function is,whereis the average rotational period,is thedispersionof periods.

References

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  1. ^abcdefgYoshida, F.; Nakamura, T (2005)."Size distribution of faint L4 Trojan asteroids".The Astronomical Journal.130(6): 2900–11.Bibcode:2005AJ....130.2900Y.doi:10.1086/497571.
  2. ^abcdefghNicholson, Seth B. (1961). "The Trojan asteroids".Astronomical Society of the Pacific Leaflets.8(381): 239–46.Bibcode:1961ASPL....8..239N.
  3. ^ab"Trojan Minor Planets".Minor Planet Center.Archivedfrom the original on 29 June 2017.Retrieved14 October2018.
  4. ^Tedesco, E. F.; Desert, F.-X. (2002)."The Infrared Space Observatory Deep Asteroid Search".The Astronomical Journal.123(4): 2070–2082.Bibcode:2002AJ....123.2070T.doi:10.1086/339482.
  5. ^abcdefghijklmJewitt, David C.; Sheppard, Scott; Porco, Carolyn C. (2004)."Jupiter's Outer Satellites and Trojans"(PDF).In Bagenal, Fran; Dowling, Timothy E.; McKinnon, William B. (eds.).Jupiter: The Planet, Satellites and Magnetosphere.Cambridge University Press.S2CID53962019.Archived from the original on 9 November 2019.Retrieved30 April2021.{{cite book}}:CS1 maint: bot: original URL status unknown (link)
  6. ^Dotto, E; Fornasier, S; Barucci, M.A; Licandr o, J; Boehnhardt, H; Hainaut, O; Marzari, F; De Bergh, C; De Luise, F (2006). "The surface composition of Jupiter Trojans: Visible and near-infrared survey of dynamical families".Icarus.183(2): 420–434.Bibcode:2006Icar..183..420D.doi:10.1016/j.icarus.2006.02.012.
  7. ^Sheppard, S. S.; C. A. Trujillo (28 July 2006)."A thick cloud of Neptune Trojans and their colors"(PDF).Science.313(5786). New York: 511–514.Bibcode:2006Sci...313..511S.doi:10.1126/science.1127173.OCLC110021198.PMID16778021.S2CID35721399.Archived fromthe original(PDF)on 12 April 2020.
  8. ^"NASA's WISE Mission Finds First Trojan Asteroid Sharing Earth's Orbit 27 July 2011".Archivedfrom the original on 2 May 2017.Retrieved29 July2011.
  9. ^Connors, Martin; Wiegert, Paul; Veillet, Christian (28 July 2011). "Earth's Trojan asteroid".Nature.475(7357): 481–483.Bibcode:2011Natur.475..481C.doi:10.1038/nature10233.PMID21796207.S2CID205225571.
  10. ^abcdefghijkMarzari, F.; Scholl, H.; Murray C.; Lagerkvist C. (2002)."Origin and Evolution of Trojan Asteroids"(PDF).Asteroids III.Tucson, Arizona: University of Arizona Press. pp. 725–38.Archived(PDF)from the original on 6 June 2011.Retrieved17 January2009.
  11. ^abcdefgJewitt, David C.; Trujillo, Chadwick A.; Luu, Jane X. (2000). "Population and size distribution of small Jovian Trojan asteroids".The Astronomical Journal.120(2): 1140–7.arXiv:astro-ph/0004117.Bibcode:2000AJ....120.1140J.doi:10.1086/301453.S2CID119450236.
  12. ^abBrian G. Marsden (1 October 1999)."The Earliest Observation of a Trojan".Harvard-Smithsonian Center for Astrophysics (CfA).Archivedfrom the original on 14 November 2008.Retrieved20 January2009.
  13. ^Einarsson, Sturla (1913). "The Minor Planets of the Trojan Group".Publications of the Astronomical Society of the Pacific.25(148): 131–3.Bibcode:1913PASP...25..131E.doi:10.1086/122216.S2CID122428016.
  14. ^abWyse, A. B.(1938). "The Trojan group".Astronomical Society of the Pacific Leaflets.3(114): 113–19.Bibcode:1938ASPL....3..113W.
  15. ^abcdefFernandes, Yanga R.; Sheppard, Scott S.; Jewitt, David C. (2003). "The albedo distribution of Jovian Trojan asteroids".The Astronomical Journal.126(3): 1563–1574.Bibcode:2003AJ....126.1563F.CiteSeerX10.1.1.7.5611.doi:10.1086/377015.S2CID15977388.
  16. ^"List of Jupiter trojans".Minor Planet Center.Archivedfrom the original on 12 June 2018.Retrieved14 October2018.
  17. ^"Trojan Asteroids".Cosmos.Swinburne University of Technology.Archivedfrom the original on 23 June 2017.Retrieved13 June2017.
  18. ^"MPEC 2020-T164".minorplanetcenter.net.Retrieved20 July2024.
  19. ^abcFernández, Y. R.; Jewitt, D.; Ziffer, J. E. (2009). "Albedos of Small Jovian Trojans".The Astronomical Journal.138(1): 240–250.arXiv:0906.1786.Bibcode:2009AJ....138..240F.doi:10.1088/0004-6256/138/1/240.S2CID5592793.
  20. ^abNakamura, Tsuko; Yoshida, Fumi (2008)."A New Surface Density Model of Jovian Trojans around Triangular Libration Points".Publications of the Astronomical Society of Japan.60(2): 293–296.Bibcode:2008PASJ...60..293N.doi:10.1093/pasj/60.2.293.
  21. ^Merline, W. J. (2001)."IAUC 7741: 2001fc; S/2001 (617) 1; C/2001 T1, C/2001 T2".Archivedfrom the original on 19 July 2011.Retrieved25 October2010.
  22. ^abMarchis, Franck; Hestroffer, Daniel; Descamps, Pascal; et al. (2006). "A low density of 0.8 g cm−3for the Trojan binary asteroid 617 Patroclus ".Nature.439(7076): 565–567.arXiv:astro-ph/0602033.Bibcode:2006Natur.439..565M.doi:10.1038/nature04350.PMID16452974.S2CID4416425.
  23. ^"IAUC 8732: S/2006 (624) 1".Archivedfrom the original on 19 July 2011.Retrieved23 July2006.(Satellite Discovery)
  24. ^abcLacerda, Pedro; Jewitt, David C. (2007). "Densities of Solar System Objects from Their Rotational Light Curves".The Astronomical Journal.133(4): 1393–1408.arXiv:astro-ph/0612237.Bibcode:2007AJ....133.1393L.doi:10.1086/511772.S2CID17735600.
  25. ^abcdeBarucci, M.A.; Kruikshank, D.P.; Mottola S.; Lazzarin M. (2002). "Physical Properties of Trojan and Centaur Asteroids".Asteroids III.Tucson, Arizona: University of Arizona Press. pp. 273–87.
  26. ^Molnar, Lawrence A.; Haegert, Melissa J.; Hoogeboom, Kathleen M. (April 2008). "Lightcurve Analysis of an Unbiased Sample of Trojan Asteroids".The Minor Planet Bulletin.35(2). Association of Lunar and Planetary Observers: 82–84.Bibcode:2008MPBu...35...82M.OCLC85447686.
  27. ^Yang, Bin; Jewitt, David (2007)."Spectroscopic Search for Water Ice on Jovian Trojan Asteroids".The Astronomical Journal.134(1): 223–228.Bibcode:2007AJ....134..223Y.doi:10.1086/518368.Retrieved19 January2009.
  28. ^Dotto, E.; Fornasier, S.; Barucci, M. A.; et al. (August 2006). "The surface composition of Jupiter trojans: Visible and near-infrared survey of dynamical families".Icarus.183(2): 420–434.Bibcode:2006Icar..183..420D.doi:10.1016/j.icarus.2006.02.012.
  29. ^Marzari, F.; Scholl, H. (1998). "The growth of Jupiter and Saturn and the capture of Trojans".Astronomy and Astrophysics.339:278–285.Bibcode:1998A&A...339..278M.
  30. ^Pirani, S.; Johansen, A.; Bitsch, B.; Mustill, A. J.; Turrini, D. (2019). "Consequences of planetary migration on the minor bodies of the early solar system".Astronomy & Astrophysics.623:A169.arXiv:1902.04591.Bibcode:2019A&A...623A.169P.doi:10.1051/0004-6361/201833713.S2CID119546182.
  31. ^Levison, Harold F.; Morbidelli, Alessandro; Van Laerhoven, Christa; et al. (2007). "Origin of the Structure of the Kuiper Belt during a Dynamical Instability in the Orbits of Uranus and Neptune".Icarus.196(1): 258–273.arXiv:0712.0553.Bibcode:2008Icar..196..258L.doi:10.1016/j.icarus.2007.11.035.S2CID7035885.
  32. ^Morbidelli, A.; Levison, H. F.; Tsiganis, K.; Gomes, R. (26 May 2005)."Chaotic capture of Jupiter's Trojan asteroids in the early Solar System"(PDF).Nature.435(7041): 462–465.Bibcode:2005Natur.435..462M.doi:10.1038/nature03540.OCLC112222497.PMID15917801.S2CID4373366.Archived fromthe original(PDF)on 31 July 2009.Retrieved19 January2009.
  33. ^abNesvorný, David; Vokrouhlický, David; Morbidelli, Alessandro (2013). "Capture of Trojans by Jumping Jupiter".The Astrophysical Journal.768(1): 45.arXiv:1303.2900.Bibcode:2013ApJ...768...45N.doi:10.1088/0004-637X/768/1/45.S2CID54198242.
  34. ^Robutal, P.; Gabern, F.; Jorba A. (2005)."The observed Trojans and the global dynamics around the lagrangian points of the sun–jupiter system"(PDF).Celestial Mechanics and Dynamical Astronomy.92(1–3): 53–69.Bibcode:2005CeMDA..92...53R.doi:10.1007/s10569-004-5976-y.S2CID5759776.Archived fromthe original(PDF)on 31 July 2009.
  35. ^Kleomenis Tsiganis; Harry Varvoglis; Rudolf Dvorak (April 2005). "Chaotic Diffusion And Effective Stability of Jupiter trojans".Celestial Mechanics and Dynamical Astronomy.92(1–3). Springer: 71–87.Bibcode:2005CeMDA..92...71T.doi:10.1007/s10569-004-3975-7.S2CID123648472.
  36. ^abLevison, Harold F.; Shoemaker, Eugene M.; Shoemaker, Carolyn S. (1997). "Dynamical evolution of Jupiter's Trojan asteroids".Nature.385(6611): 42–44.Bibcode:1997Natur.385...42L.doi:10.1038/385042a0.S2CID4323757.
  37. ^Northon, Karen (4 January 2017)."NASA Selects Two Missions to Explore the Early Solar System".NASA.Archivedfrom the original on 5 January 2017.Retrieved5 January2017.
  38. ^"Tour".Lucy Mission Website.NASA.Archivedfrom the original on 8 September 2018.Retrieved5 October2021.
  39. ^Dreier, Casey; Lakdawalla, Emily (30 September 2015)."NASA announces five Discovery proposals selected for further study".The Planetary Society.Archivedfrom the original on 2 October 2015.Retrieved1 October2015.
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