2020
DOI: 10.1002/essoar.10503201.1
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Macroporosity and Grain Density of Rubble Pile Asteroid (162173) Ryugu

Abstract: • Ryugu's large bulk porosity is distributed between intrinsic boulder microporosity and macroporosity due to void spaces in-between boulders. • We use the boulder size-frequency distribution as observed on the surface together with mixing models to estimate Ryugu's macroporosity. • We find that macroporosity is 16±3 %, indicating that Ryugu's large bulk porosity of close to 50 % is governed by microporosity.

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Cited by 2 publications
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“…Provided that the sample is representative, the global average density (bulk density) of Ryugu is 1190 ± 20 kg m -3 [8] , and indicates macro-porosity of ~10% which is contrary to large macro-porosities required for primitive asteroids when typical meteoritic density is assumed 28 , provided that the returned samples collected from the two sampling sites on the surface of Ryugu represent the entire materials of Ryugu. The low macro-porosity of Ryugu is probably consistent with the packing model using the size-frequency distribution of Ryugu 29 . A difference in density distribution is found between Chambers A and C, with particles denser than 1800 kg m -3 [9] (> 2σ) only found in Chamber A, that being within the density range of typical meteorites found on Earth 12 , and indicating Ryugu might consist of a mixture of particles from different origins 30 or different degree of alteration processes in the parent bodies 5,31 .…”
Section: Main Textsupporting
confidence: 76%
“…Provided that the sample is representative, the global average density (bulk density) of Ryugu is 1190 ± 20 kg m -3 [8] , and indicates macro-porosity of ~10% which is contrary to large macro-porosities required for primitive asteroids when typical meteoritic density is assumed 28 , provided that the returned samples collected from the two sampling sites on the surface of Ryugu represent the entire materials of Ryugu. The low macro-porosity of Ryugu is probably consistent with the packing model using the size-frequency distribution of Ryugu 29 . A difference in density distribution is found between Chambers A and C, with particles denser than 1800 kg m -3 [9] (> 2σ) only found in Chamber A, that being within the density range of typical meteorites found on Earth 12 , and indicating Ryugu might consist of a mixture of particles from different origins 30 or different degree of alteration processes in the parent bodies 5,31 .…”
Section: Main Textsupporting
confidence: 76%