Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/114650
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorRen, J-
dc.creatorWu, B-
dc.creatorHesse, MA-
dc.creatorLi, H-
dc.creatorLiu, Y-
dc.creatorWang, X-
dc.date.accessioned2025-08-18T03:02:36Z-
dc.date.available2025-08-18T03:02:36Z-
dc.identifier.urihttp://hdl.handle.net/10397/114650-
dc.language.isoenen_US
dc.publisherEDP Sciencesen_US
dc.rights© The Authors 2024en_US
dc.rightsOpen Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. A62, page 1 of 11 This article is published in open access under the Subscribe to Open model. Subscribe to A&A to support open access publication.en_US
dc.rightsThe following publication Ren, J., Wu, B., Hesse, M. A., Li, H., Liu, Y., & Wang, X. (2024). Surface dynamics of small fast-rotating asteroids: Analysis of possible regolith on asteroid 2016 HO3. A&A, 692, A62 is available at https://doi.org/10.1051/0004-6361/202451407.en_US
dc.subjectMinor planets, asteroids: generalen_US
dc.subjectMinor planets, asteroids: individual: 2016 HO3en_US
dc.subjectMinor planets, asteroids: individual: 469219 Kamo-oalewaen_US
dc.titleSurface dynamics of small fast-rotating asteroids : analysis of possible regolith on asteroid 2016 HO3en_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume692-
dc.identifier.doi10.1051/0004-6361/202451407-
dcterms.abstractThe Chinese Tianwen-2 mission is planned to explore and sample the near-Earth asteroid 2016 HO3, also named 469219 Kamo’oalewa. This paper intends to answer the question of whether 2016 HO3 has any regolith. A 3D model of an irregular shape was reconstructed from light curve data of 2016 HO3, with simulated impact craters embedded on its surface. We used numerical simulations to calculate the acceleration from gravity, fast rotation, and the van der Waals cohesive force. We found that the poles have a higher chance of hosting regolith, and the regolith may also rest on the walls of craters that face toward the rotation axis, making them potential sample collection sites. On the surface of 2016 HO3, the van der Waals force is strong enough to hold particles smaller than several centimeters against centrifugal force. Furthermore, we compare a pair of transient processes: thermal fatigue, which generates small particles, and micro-impacts, which remove the surface mass. Thermal fatigue is at least comparable to, and perhaps more efficient than, micro-impacts for 2016 HO3. Therefore, it is highly possible that regolith exists on the surface of 2016 HO3.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationAstronomy and astrophysics, Dec. 2024, v. 692, A62-
dcterms.isPartOfAstronomy and astrophysics-
dcterms.issued2024-12-
dc.identifier.scopus2-s2.0-85211502825-
dc.identifier.eissn1432-0746-
dc.identifier.artnA62-
dc.description.validate202508 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Othersen_US
dc.description.fundingSourceRGCen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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