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  • 1
    In: Science Advances, American Association for the Advancement of Science (AAAS), Vol. 8, No. 46 ( 2022-11-18)
    Abstract: The Hayabusa2 metal-sealed container successfully returned extraterrestrial He and Ne as a gas phase from the asteroid Ryugu.
    Type of Medium: Online Resource
    ISSN: 2375-2548
    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2022
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  • 2
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 379, No. 6634 ( 2023-02-24)
    Abstract: The Hayabusa2 spacecraft retrieved surface and subsurface samples from the carbonaceous near-Earth asteroid (162173) Ryugu, which was expected to be enriched in volatile species. The samples were collected from two locations, one undisturbed surface and the other including material excavated by an artificial impact. Unlike meteorites, these samples have experienced minimal alteration by Earth’s atmosphere. Ryugu is thought to have formed from material ejected (by an impact) from a parent body, which had experienced aqueous alteration (reactions with liquid water) ~4.56 billion years (Gyr) ago. Ryugu’s orbit later migrated from the main asteroid belt to become a near-Earth asteroid. RATIONALE Noble gases and nitrogen isotopes in Ryugu grains are inherited from Ryugu’s parent body and potentially provide information about the source of Earth’s volatile elements. Noble gas isotopes can also be used to assess the orbital evolution and recent surface activities of Ryugu. We pelletized ~0.8-mm-diameter Ryugu grains and investigated their mineralogy before carrying out isotope measurements. We measured the concentrations and isotopic compositions of noble gases and nitrogen, extracted by stepped heating, with mass spectrometers. RESULTS The mineralogy of the Ryugu grains is similar to Ivuna-type carbonaceous (CI) chondrite meteorites. Fine-grained hydrous silicates (phyllosilicates), produced through aqueous alteration of primary minerals, compose the major fraction of the samples. This is consistent with infrared spectroscopic observations of the asteroid. Iron oxide, iron sulfides, and carbonates are also found within the matrix. Noble gas isotopes are dominated by primordially trapped gases. Their abundances are mostly similar to the highest found in a CI chondrite, with some grains having several times higher concentrations than the highest CI value. Isotopic compositions and concentrations of nitrogen vary between the Ryugu grains, with divergence from the CI chondrite composition. The nitrogen concentrations in four Ryugu grains are one-half to one-third the CI values, and the 15 N/ 14 N ratio is also lower. The Ryugu grains with compositions farthest from the CI values are similar to the composition of a dehydrated CI chondrite. Only two surface samples, out of the 16 Ryugu grains measured, have clear signs of noble gases derived from solar wind (SW). Their abundances correspond to SW exposure durations of ≳3500 and ≳250 years at the current orbit, whereas most of the grains were exposed for ≳1 to ≳50 years. Cosmic ray–produced 21 Ne concentrations vary, with no systematic difference between the sample collection sites. The estimated cosmic ray exposure (CRE) ages for the surface and subsurface samples are 5.3 ± 0.9 and 5.2 ± 0.8 million years (Myr), assuming irradiations at 2 to 5 g cm −2 and 150 g cm −2 , respectively. This is consistent with the expected surface residence time under near-Earth impact rates. We infer that Ryugu’s orbit migrated from the main asteroid belt to the near-Earth region ~5 Myr ago. About 30% of cosmogenic 21 Ne, corresponding to a CRE age of ~1 Myr, was released in gas-extraction steps at 100°C, indicating that the Ryugu samples have not experienced heating above 100°C within the past 1 Myr. Previous studies have suggested that Ryugu experienced an orbital excursion much closer to the Sun. If this is the case, this excursion must have occurred ≳1 Myr ago. CONCLUSION The mineralogical and noble gas measurements show that the Ryugu samples are similar to CI chondrites. The nitrogen data indicate a heterogeneous distribution of nitrogen-carrying materials with different compositions, one of which has been lost from Ryugu grains to varying degrees. The CRE age of ~5 Myr and the implanted SW are records of the recent irradiation at the current near-Earth orbit of Ryugu. Inferred formation and history of Ryugu. Ryugu’s parent body formed in the early Solar System, incorporating primordial noble gases and nitrogen, followed by aqueous alteration ~4.56 Gyr ago. Ryugu formed from the accumulation of fragments of the parent body ejected by an impact, at an unknown date. Ryugu migrated to its current near-Earth orbit ~5 Myr ago. Ryugu might have experienced another change in orbit, bringing it closer to the Sun (“Path A”), or remained in the same near-Earth orbit (“Path B”).
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
    RVK:
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2023
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    SSG: 11
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  • 3
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 379, No. 6634 ( 2023-02-24)
    Abstract: Surface material from the near-Earth carbonaceous (C-type) asteroid (162173) Ryugu was collected and brought to Earth by the Hayabusa2 spacecraft. Ryugu is a dark, primitive asteroid containing hydrous minerals that are similar to the most hydrated carbonaceous meteorites. C-type asteroids are common in the asteroid belt and have been proposed as the parent bodies of carbonaceous meteorites. The samples of Ryugu provide an opportunity to investigate organic compounds for comparison with those from carbonaceous meteorites. Unlike meteorites, the Ryugu samples were collected and delivered for study under controlled conditions, reducing terrestrial contamination and the effects of atmospheric entry. RATIONALE Primitive carbonaceous chondrite meteorites are known to contain a variety of soluble organic molecules (SOMs), including prebiotic molecules such as amino acids. Meteorites might have delivered amino acids and other prebiotic organic molecules to the early Earth and other rocky planets. Organic matter in the Ryugu samples is the product of physical and chemical processes that occurred in the interstellar medium, the protosolar nebula, and/or on the planetesimal that became Ryugu’s parent body. We investigated SOMs in Ryugu samples principally using mass spectrometry coupled with liquid or gas chromatography. RESULTS We identified numerous organic molecules in the Ryugu samples. Mass spectroscopy detected hundreds of thousands of ion signals, which we assigned to ~20,000 elementary compositions consisting of carbon, hydrogen, nitrogen, oxygen, and/or sulfur. Fifteen amino acids, including glycine, alanine, and α-aminobutyric acid, were identified. These were present as racemic mixtures (equal right- and left-handed abundances), consistent with an abiotic origin. Aliphatic amines (such as methylamine) and carboxylic acids (such as acetic acid) were also detected, likely retained on Ryugu as organic salts. The presence of aromatic hydrocarbons, including alkylbenzenes, fluoranthene, and pyrene, implies hydrothermal processing on Ryugu’s parent body and/or presolar synthesis in the interstellar medium. Nitrogen-containing heterocyclic compounds were identified as their alkylated homologs, which could have been synthesized from simple aldehydes and ammonia. In situ analysis of a grain surface showed heterogeneous spatial distribution of alkylated homologs of nitrogen- and/or oxygen-containing compounds. CONCLUSION The wide variety of molecules identified indicates that prolonged chemical processes contributed to the synthesis of soluble organics on Ryugu or its parent body. The highly diverse mixture of SOMs in the samples resembles that seen in some carbonaceous chondrites. However, the SOM concentration in Ryugu is less than that in moderately aqueously altered CM (Mighei-type) chondrites, being more similar to that seen in warm aqueously altered CI (Ivuna-type) chondrites. The chemical diversity with low SOM concentration in Ryugu is consistent with aqueous organic chemistry at modest temperatures on Ryugu’s parent asteroid. The samples collected from the surface of Ryugu were exposed to the hard vacuum of space, energetic particle irradiation, heating by sunlight, and micrometeoroid impacts, but the SOM is still preserved, likely by being associated with minerals. The presence of prebiotic molecules on the asteroid surface suggests that these molecules can be transported throughout the Solar System. SOMs detected in surface samples of asteroid Ryugu. Chemical structural models are shown for example molecules from several classes identified in the Ryugu samples. Gray balls are carbon, white are hydrogen, red are oxygen, and blue are nitrogen. Clockwise from top: amines (represented by ethylamine), nitrogen-containing heterocycles (pyridine), a photograph of the sample vials for analysis, polycyclic aromatic hydrocarbons (PAHs) (pyrene), carboxylic acids (acetic acid), and amino acids (β-alanine). The central hexagon shows a photograph of the Ryugu sample in the sample collector of the Hayabusa2 spacecraft. The background image shows Ryugu in a photograph taken by Hayabusa2. CREDIT: JAXA, University of Tokyo, Kochi University, Rikkyo University, Nagoya University, Chiba Institute of Technology, Meiji University, University of Aizu, AIST, NASA, Dan Gallagher.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
    RVK:
    RVK:
    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2023
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    detail.hit.zdb_id: 2066996-3
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    SSG: 11
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  • 4
    In: Planetary and Space Science, Elsevier BV, Vol. 219 ( 2022-09), p. 105519-
    Type of Medium: Online Resource
    ISSN: 0032-0633
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2022
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    SSG: 16,12
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  • 5
    In: Nature Astronomy, Springer Science and Business Media LLC, Vol. 6, No. 2 ( 2021-12-20), p. 214-220
    Abstract: C-type asteroids 1 are considered to be primitive small Solar System bodies enriched in water and organics, providing clues to the origin and evolution of the Solar System and the building blocks of life. C-type asteroid 162173 Ryugu has been characterized by remote sensing 2–7 and on-asteroid measurements 8,9 with Hayabusa2 (ref.  10 ). However, the ground truth provided by laboratory analysis of returned samples is invaluable to determine the fine properties of asteroids and other planetary bodies. We report preliminary results of analyses on returned samples from Ryugu of the particle size distribution, density and porosity, spectral properties and textural properties, and the results of a search for Ca–Al-rich inclusions (CAIs) and chondrules. The bulk sample mainly consists of rugged and smooth particles of millimetre to submillimetre size, confirming that the physical and chemical properties were not altered during the return from the asteroid. The power index of its size distribution is shallower than that of the surface boulder observed on Ryugu 11 , indicating differences in the returned Ryugu samples. The average of the estimated bulk densities of Ryugu sample particles is 1,282 ± 231 kg m −3 , which is lower than that of meteorites 12 , suggesting a high microporosity down to the millimetre scale, extending centimetre-scale estimates from thermal measurements 5,9 . The extremely dark optical to near-infrared reflectance and spectral profile with weak absorptions at 2.7 and 3.4 μm imply a carbonaceous composition with indigenous aqueous alteration, matching the global average of Ryugu 3,4 and confirming that the sample is representative of the asteroid. Together with the absence of submillimetre CAIs and chondrules, these features indicate that Ryugu is most similar to CI chondrites but has lower albedo, higher porosity and more fragile characteristics.
    Type of Medium: Online Resource
    ISSN: 2397-3366
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2021
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  • 6
    In: Nature Astronomy, Springer Science and Business Media LLC
    Abstract: Without a protective atmosphere, space-exposed surfaces of airless Solar System bodies gradually experience an alteration in composition, structure and optical properties through a collective process called space weathering. The return of samples from near-Earth asteroid (162173) Ryugu by Hayabusa2 provides the first opportunity for laboratory study of space-weathering signatures on the most abundant type of inner solar system body: a C-type asteroid, composed of materials largely unchanged since the formation of the Solar System. Weathered Ryugu grains show areas of surface amorphization and partial melting of phyllosilicates, in which reduction from Fe 3+ to Fe 2+ and dehydration developed. Space weathering probably contributed to dehydration by dehydroxylation of Ryugu surface phyllosilicates that had already lost interlayer water molecules and to weakening of the 2.7 µm hydroxyl (–OH) band in reflectance spectra. For C-type asteroids in general, this indicates that a weak 2.7 µm band can signify space-weathering-induced surface dehydration, rather than bulk volatile loss.
    Type of Medium: Online Resource
    ISSN: 2397-3366
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2022
    detail.hit.zdb_id: 2879712-7
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  • 7
    In: Astrodynamics, Springer Science and Business Media LLC, Vol. 4, No. 4 ( 2020-12), p. 349-375
    Type of Medium: Online Resource
    ISSN: 2522-008X , 2522-0098
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2020
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  • 8
    In: Nature Astronomy, Springer Science and Business Media LLC, Vol. 6, No. 10 ( 2022-08-15), p. 1163-1171
    Abstract: Volatile and organic-rich C-type asteroids may have been one of the main sources of Earth’s water. Our best insight into their chemistry is currently provided by carbonaceous chondritic meteorites, but the meteorite record is biased: only the strongest types survive atmospheric entry and are then modified by interaction with the terrestrial environment. Here we present the results of a detailed bulk and microanalytical study of pristine Ryugu particles, brought to Earth by the Hayabusa2 spacecraft. Ryugu particles display a close compositional match with the chemically unfractionated, but aqueously altered, CI (Ivuna-type) chondrites, which are widely used as a proxy for the bulk Solar System composition. The sample shows an intricate spatial relationship between aliphatic-rich organics and phyllosilicates and indicates maximum temperatures of ~30 °C during aqueous alteration. We find that heavy hydrogen and nitrogen abundances are consistent with an outer Solar System origin. Ryugu particles are the most uncontaminated and unfractionated extraterrestrial materials studied so far, and provide the best available match to the bulk Solar System composition.
    Type of Medium: Online Resource
    ISSN: 2397-3366
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2022
    detail.hit.zdb_id: 2879712-7
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  • 9
    In: Space Science Reviews, Springer Science and Business Media LLC, Vol. 216, No. 7 ( 2020-10)
    Type of Medium: Online Resource
    ISSN: 0038-6308 , 1572-9672
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2020
    detail.hit.zdb_id: 2017804-9
    detail.hit.zdb_id: 2561549-X
    SSG: 16,12
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  • 10
    In: Communications Earth & Environment, Springer Science and Business Media LLC, Vol. 4, No. 1 ( 2023-09-27)
    Abstract: Returned samples from Cb-type asteroid (162173) Ryugu exhibit very dark spectra in visible and near-infrared ranges, generally consistent with the Hayabusa2 observations. A critical difference is that a structural water absorption of hydrous silicates is around twice as deep in the returned samples compared with those of Ryugu’s surface, suggesting Ryugu surface is more dehydrated. Here we use laboratory experiments data to indicate the spectral differences between returned samples and asteroid surface are best explained if Ryugu surface has (1) higher porosity, (2) larger particle size, and (3) more space-weathered condition, with the last being the most effective. On Ryugu, space weathering by micrometeoroid bombardments promoting dehydration seem to be more effective than that by solar-wind implantation. Extremely homogeneous spectra of the Ryugu’s global surface is in contrast with the heterogeneous S-type asteroid (25143) Itokawa’s spectra, which suggests space weathering has proceeded more rapidly on Cb-type asteroids than S-type asteroids.
    Type of Medium: Online Resource
    ISSN: 2662-4435
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2023
    detail.hit.zdb_id: 3037243-4
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