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dc.contributor.authorEmery, Joshua P.
dc.contributor.authorBinzel, Richard P.
dc.contributor.authorBritt, Daniel T.
dc.contributor.authorBrown, Michael E.
dc.contributor.authorHowett, Carly J. A.
dc.contributor.authorMartin, Audrey C.
dc.contributor.authorMelita, Mario D.
dc.contributor.authorSouza-Feliciano, Ana Carolina
dc.contributor.authorWong, Ian
dc.date.accessioned2024-04-01T16:40:37Z
dc.date.available2024-04-01T16:40:37Z
dc.date.issued2024-03-25
dc.identifier.issn0038-6308
dc.identifier.issn1572-9672
dc.identifier.urihttps://hdl.handle.net/1721.1/153983
dc.description.abstractThe Jupiter Trojan asteroids are a key population for understanding the chemical and dynamical evolution of the Solar System. Surface compositions of Trojans, in turn, provide crucial information for reconstructing their histories. NASA’s Lucy mission will soon complete the first spacecraft reconnaissance of this population. This review summarizes the current state of knowledge of Trojan surface compositions and looks ahead to expected advances in that knowledge from Lucy. Surface compositions of Trojans remain uncertain due to a relative lack of diagnostic absorption features, though dedicated observations have begun to provide some clues to compositions. Trojans have uniformly low albedos, with a population average of ∼5.3%, and red spectral slopes at ultraviolet, visible, and near-infrared wavelengths. A bimodality of spectral slopes has been detected and confirmed across all these wavelengths, and the ratio of “less-red” to “red” Trojans increases with decreasing size. A broad absorption at ∼3.1 μm in some less-red Trojans may indicate the presence of N-H bearing material. Mid-infrared emissivity spectra reveal the presence of fine-grained anhydrous silicates on the surfaces. The meteorite collection contains no identifiable analogs to Trojan asteroids. Among small body populations, some Main Belt asteroids, comets, irregular satellites, and Centaurs provide reasonable spectral matches, supporting some genetic relationships among some members of these groups. The cause of the observed spectral properties remains uncertain, but recent suggestions include a combination of volatile ice sublimation and space weathering or a combination of impact gardening and space weathering. The Lucy mission will provide detailed compositional analysis of (3548) Eurybates, (15094) Polymele, (11351) Leucus, (21900) Orus, and (617) Patroclus-Menoetius, a suite of targets that sample the diversity among the Trojan population along several dimensions. With these flybys, the Lucy mission is poised to resolve many of the outstanding questions regarding Trojan surface compositions, thereby revealing how the Trojans formed and evolved and providing a clearer view of Solar System history.en_US
dc.publisherSpringer Science and Business Media LLCen_US
dc.relation.isversionof10.1007/s11214-024-01060-7en_US
dc.rightsCreative Commons Attributionen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.sourceSpringer Netherlandsen_US
dc.subjectSpace and Planetary Scienceen_US
dc.subjectAstronomy and Astrophysicsen_US
dc.titleSurface Compositions of Trojan Asteroidsen_US
dc.typeArticleen_US
dc.identifier.citationSpace Science Reviews. 2024 Mar 25;220(3):28en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.contributor.departmentMassachusetts Institute of Technology. Department of Aeronautics and Astronautics
dc.relation.journalSpace Science Reviewsen_US
dc.identifier.mitlicensePUBLISHER_CC
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2024-03-31T03:16:59Z
dc.language.rfc3066en
dc.rights.holderThe Author(s)
dspace.embargo.termsN
dspace.date.submission2024-03-31T03:16:59Z
mit.journal.volume220en_US
mit.journal.issue3en_US
mit.licensePUBLISHER_CC
mit.metadata.statusAuthority Work and Publication Information Neededen_US


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