Heterogeneous mass distribution of the rubble-pile asteroid (101955) Bennu.
Daniel J ScheeresA S FrenchP TricaricoSteven R ChesleyY TakahashiD FarnocchiaJ W McMahonD N BrackA B DavisRonald-Louis BallouzErica R JawinBenjamin RozitisJoshua P EmeryAndrew J RyanRyan S ParkB P RushN MastrodemosB M KennedyJ BelleroseD P LubeyDianna VelezA T VaughanJason M LeonardJ GeeraertB PageP G AntreasianErwan MazaricoK GetzandannerD RowlandsMichael MoreauJ SmallD E HighsmithSander GoossensEric E PalmerJ R WeirichR W GaskellOlivier S BarnouinMichael G DalyJ A SeabrookManar Al AsadLydia PhilpottCatherine L JohnsonChristine M HartzellVictoria E HamiltonPatrick MichelKevin J WalshMichael C NolanDante S LaurettaPublished in: Science advances (2020)
The gravity field of a small body provides insight into its internal mass distribution. We used two approaches to measure the gravity field of the rubble-pile asteroid (101955) Bennu: (i) tracking and modeling the spacecraft in orbit about the asteroid and (ii) tracking and modeling pebble-sized particles naturally ejected from Bennu's surface into sustained orbits. These approaches yield statistically consistent results up to degree and order 3, with the particle-based field being statistically significant up to degree and order 9. Comparisons with a constant-density shape model show that Bennu has a heterogeneous mass distribution. These deviations can be modeled with lower densities at Bennu's equatorial bulge and center. The lower-density equator is consistent with recent migration and redistribution of material. The lower-density center is consistent with a past period of rapid rotation, either from a previous Yarkovsky-O'Keefe-Radzievskii-Paddack cycle or arising during Bennu's accretion following the disruption of its parent body.
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