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Fine-grained regolith loss on sub-km asteroids

Abstract

Fine-grained regolith, a surface layer of unconsolidated granular material, has been considered to cover the surfaces of airless bodies and determine their spectral and thermophysical properties. However, surfaces of asteroids visited by recent sample return missions are dominated by centimetre- to metre-sized boulders, indicating an active fine-grained regolith removal process at work. To understand asteroid regolith evolution, we apply recent space and laboratory experimental results to simulate regolith fragmentation processes, loss by impact ejecta, and electrostatic removal of fine-grained regolith. Here we show that coarse, boulder-rich scenery probably emerges on kilometre-sized and smaller asteroids within a few million years, as the electrostatic removal of fine-grained regolith dominates production by fragmentation. Surface thermal inertia enhancement associated with fine-grained regolith loss on small main-belt asteroids increases the Yarkovsky drift and the probability of orbital excursion to the near-Earth environment through resonances with giant planets. We suggest that the competition between electrostatic erosion and space weathering shapes the appearance of reflectance spectra of small asteroids, related to the size, spatial and spectral distributions of S-complex asteroids.

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Fig. 1: Regolith size distribution evolution for asteroids at 1 au heliocentric distance.
Fig. 2: Regolith age and processing rate evolution for asteroids at 1 au heliocentric distance.
Fig. 3: Regolith end-state statistics and fine-grained regolith removal timescale as functions of body radius and heliocentric distance.

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Data availability

Source data are provided with this paper. Modelling results presented in this work can be found in the source data files.

Code availability

Parameters and equations needed to perform the calculation are described in Methods. The codes used in this study are available from the corresponding author upon reasonable request.

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Acknowledgements

This work is supported by the NASA/ROSES NNH15ZDA001N-SSW Solar System Workings programme (grant number NNX16AO81G) and the NASA/SSERVI Institute for Modeling Plasma, Atmospheres and Cosmic Dust. H.-W.H. thanks M. Delbo and W.-H. Ip for fruitful discussions and T.-W. Liu, C.-Y. Wang, Li. Hsu and Lu. Hsu for their support.

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H.-W.H., X.W. and M.H. coordinated this study. H.-W.H. performed the model calculation. A.C., N.H. and X.W. provided experimental results to perform the calculation. All authors contributed to discussions and editing the manuscript.

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Correspondence to Hsiang-Wen Hsu.

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Nature Astronomy thanks Seiji Sugita and Christine Hartzell for their contribution to the peer review of this work.

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Extended data

Extended Data Fig. 1 Regolith Size Distribution Evolution Modeling.

A schematic illustrates the three processes considered in shaping the regolith size evolution on airless bodies.

Extended Data Fig. 2 Size distribution of electrostatically lofted particles from laboratory experiments.

The cumulative grain size distribution of lofted particles derived from laboratory experiments based on the results shown in Figure S2B in the Supporting Information of Wang et al. (2016). Two power-law size distributions are fitted to grain radius ranges 4 to 25 μm and 25 to 70 μm. The experiment was carried out using irregular shaped Mars simulants, 38 - 48 μm in diameter, under 120 eV electron beam irradiation. The fact that there are larger grains suggests the lofted grains are in form of aggregates.

Extended Data Fig. 3 Escape probability of electrostatic-lofted dust particles.

The maximum lofting speed as a function of grain size and the relation with the escape probability of an electrostatic-lofted grain from a rotating body. The particle size range considered is from 1 to 100 μm.

Extended Data Fig. 4 Observable and modeled power-law size distribution indices considering partial coverage.

The size indices derived from Ryugu and Bennu images (Michikami et al., 2019, Burke et al., 2021) and the modeling results are also shown. The dash line marks a reference for an 1-to-1 relationship between the two.

Source data

Extended Data Table 1 The nominal values and the ranges of parameters used in the regolith size distribution evolution simulation. Note that the listed rates are the maximum values for each simulation and the actual processing rates could vary depending on the regolith size distribution

Source data

Source Data Fig. 1

Modelling results.

Source Data Fig. 2

Modelling results.

Source Data Fig. 3

Modelling results.

Source Data Extended Data Fig. 4

Modelling results.

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Hsu, HW., Wang, X., Carroll, A. et al. Fine-grained regolith loss on sub-km asteroids. Nat Astron 6, 1043–1050 (2022). https://doi.org/10.1038/s41550-022-01717-9

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