研究者業績
基本情報
- 所属
- 国立研究開発法人宇宙航空研究開発機構 宇宙科学研究所 宇宙機応用工学研究系 はやぶさ2プロジェクト 准教授
- 学位
- 理学博士(1989年3月 東京大学)
- 連絡先
- yoshikawa.makoto
jaxa.jp
- J-GLOBAL ID
- 200901037361657011
- researchmap会員ID
- 1000304540
研究キーワード
6経歴
5-
2003年10月 - 現在
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1998年4月 - 2003年9月
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1991年4月 - 1998年3月
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1996年12月 - 1997年12月
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1989年4月 - 1991年3月
学歴
2-
1984年4月 - 1989年3月
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1980年4月 - 1984年3月
委員歴
9-
2020年10月 - 現在
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1994年4月 - 現在
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2013年1月 - 2015年3月
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2011年1月 - 2012年12月
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2009年 - 2011年
受賞
2-
2019年11月
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2018年12月
論文
287-
Meteoritics & Planetary Science 2024年11月25日Abstract Nucleosynthetic isotope variations are powerful tracers to determine genetic relationships between meteorites and planetary bodies. They can help to link material collected by space missions to known meteorite groups. The Hayabusa 2 mission returned samples from the Cb‐type asteroid (162173) Ryugu. The mineralogical, chemical, and isotopic characteristics of these samples show strong similarities to carbonaceous chondrites and in particular CI chondrites. The nucleosynthetic isotope compositions of Ryugu overlap with CI chondrites for several elements (e.g., Cr, Ti, Fe, and Zn). In contrast to these isotopes, which are of predominately supernovae origin, s‐process variations in Mo isotope data are similar to those of carbonaceous chondrites, but even more s‐process depleted. To further constrain the origin of this depletion and test whether this signature is also present for other s‐process elements, we report Zr isotope compositions for three bulk Ryugu samples (A0106, A0106‐A0107, C0108) collected from the Hayabusa 2 mission. The data are complemented with that of terrestrial rock reference materials, eucrites, and carbonaceous chondrites. The Ryugu samples are characterized by distinct 96Zr enrichment relative to Earth, indicative of a s‐process depletion. Such depletion is also observed for carbonaceous chondrites and eucrites, in line with previous Zr isotope work, but it is more extreme in Ryugu, as observed for Mo isotopes. Since s‐process Zr and Mo are coupled in mainstream SiC grains, these distinct s‐process variations might be due to SiC grain depletion in the analyzed materials, potentially caused by incomplete sample digestion, because the Ryugu samples were dissolved on a hotplate only to avoid high blank levels for other elements (e.g., Cr). However, local depletion of SiC grains cannot be excluded. An alternative, equally possible scenario is that aqueous alteration redistributed anomalous, s‐process‐depleted, Zr on a local scale, for example, into Ca‐phosphates or phyllosilicates.
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Science Advances 10(39) 2024年9月27日The isotopic compositions of samples returned from Cb-type asteroid Ryugu and Ivuna-type (CI) chondrites are distinct from other carbonaceous chondrites, which has led to the suggestion that Ryugu/CI chondrites formed in a different region of the accretion disk, possibly around the orbits of Uranus and Neptune. We show that, like for Fe, Ryugu and CI chondrites also have indistinguishable Ni isotope anomalies, which differ from those of other carbonaceous chondrites. We propose that this unique Fe and Ni isotopic composition reflects different accretion efficiencies of small FeNi metal grains among the carbonaceous chondrite parent bodies. The CI chondrites incorporated these grains more efficiently, possibly because they formed at the end of the disk’s lifetime, when planetesimal formation was also triggered by photoevaporation of the disk. Isotopic variations among carbonaceous chondrites may thus reflect fractionation of distinct dust components from a common reservoir, implying CI chondrites/Ryugu may have formed in the same region of the accretion disk as other carbonaceous chondrites.
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Nature Astronomy 2024年9月25日
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Nature Communications 15 7488 2024年8月29日 査読有りAbstract Primordial carbon delivered to the early earth by asteroids and meteorites provided a diverse source of extraterrestrial organics from pre-existing simple organic compounds, complex solar-irradiated macromolecules, and macromolecules from extended hydrothermal processing. Surface regolith collected by the Hayabusa2 spacecraft from the carbon-rich asteroid 162173 Ryugu present a unique opportunity to untangle the sources and processing history of carbonaceous matter. Here we show carbonaceous grains in Ryugu can be classified into three main populations defined by spectral shape: Highly aromatic (HA), Alkyl-Aromatic (AA), and IOM-like (IL). These carbon populations may be related to primordial chemistry, since C and N isotopic compositions vary between the three groups. Diffuse carbon is occasionally dominated by molecular carbonate preferentially associated with coarse-grained phyllosilicate minerals. Compared to related carbonaceous meteorites, the greater diversity of organic functional chemistry in Ryugu indicate the pristine condition of these asteroid samples.
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Geochimica et Cosmochimica Acta 379 172-183 2024年8月
MISC
499-
日本惑星科学会誌遊星人 27(4) 320-327 2018年<p> 2018年11月,「はやぶさ2」のミッションは,その前半が終了した.2018年6月27日に目的地である小惑星リュウグウに到着し,リモートセンシングによる観測は一通り終了した.また,小型ローバMINERVA-II1と小型着陸機MASCOTをリュウグウ表面に降ろすことにも成功し,これらからのデータの取得もできた.ただし,サンプルを採取するためのタッチダウンは,2019年に延期となった.これは,リュウグウ表面の至る所に岩塊が存在しており,安全に着陸できる十分に広い場所が見つからなかったため,探査機のより高精度なナビゲーションが必要になったためである.ここでは,「はやぶさ2」の誕生の経緯からミッション前半までをまとめてみることにする.</p>
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天文月報 = The astronomical herald 110(10) 645-655 2017年10月
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Space Science Reviews 208(1-4) 375-400 2017年7月1日The MASCOT Camera (MasCam) is part of the Mobile Asteroid Surface Scout (MASCOT) lander’s science payload. MASCOT has been launched to asteroid (162173) Ryugu onboard JAXA’s Hayabusa 2 asteroid sample return mission on Dec 3rd, 2014. It is scheduled to arrive at Ryugu in 2018, and return samples to Earth by 2020. MasCam was designed and built by DLR’s Institute of Planetary Research, together with Airbus-DS Germany. The scientific goals of the MasCam investigation are to provide ground truth for the orbiter’s remote sensing observations, provide context for measurements by the other lander instruments (radiometer, spectrometer and magnetometer), the orbiter sampling experiment, and characterize the geological context, compositional variations and physical properties of the surface (e.g. rock and regolith particle size distributions). During daytime, clear filter images will be acquired. During night, illumination of the dark surface is performed by an LED array, equipped with 4 × 36 monochromatic light-emitting diodes (LEDs) working in four spectral bands. Color imaging will allow the identification of spectrally distinct surface units. Continued imaging during the surface mission phase and the acquisition of image series at different sun angles over the course of an asteroid day will contribute to the physical characterization of the surface and also allow the investigation of time-dependent processes and to determine the photometric properties of the regolith. The MasCam observations, combined with the MASCOT hyperspectral microscope (MMEGA) and radiometer (MARA) thermal observations, will cover a wide range of observational scales and serve as a strong tie point between Hayabusa 2’s remote-sensing scales (10 –10 m) and sample scales (10 –10 m). The descent sequence and the close-up images will reveal the surface features over a broad range of scales, allowing an assessment of the surface’s diversity and close the gap between the orbital observations and those made by the in-situ measurements. The MasCam is mounted inside the lander slightly tilted, such that the center of its 54.8° square field-of-view is directed towards the surface at an angle of 22° with respect to the surface plane. This is to ensure that both the surface close to the lander and the horizon are observable. The camera optics is designed according to the Scheimpflug principle, thus that the entire scene along the camera’s depth of field (150 mm to infinity) is in focus. The camera utilizes a 1024 × 1024 pixel CMOS sensor sensitive in the 400–1000 nm wavelength range, peaking at 600–700 nm. Together with the f-16 optics, this yields a nominal ground resolution of 150 micron/px at 150 mm distance (diffraction limited). The camera flight model has undergone standard radiometric and geometric calibration both at the component and system (lander) level. MasCam relies on the use of wavelet compression to maximize data return within stringent mission downlink limits. All calibration and flight data products will be generated and archived in the Planetary Data System in PDS image format. 3 − 3 − 3 − 6
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宇宙航空研究開発機構特別資料 JAXA-SP-(Web) (16-011) 2017年
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日本物理学会誌 72(2) 98-104 2017年<p>1801年に最初の小惑星であるケレス(Ceres)が発見されてから200年余り経った現在,発見されている小惑星の数は70万個を超えた.探査機が接近した小惑星も10個ほどになり,地上観測では分からなかった小惑星のいろいろな特徴が見えてきた.また,日本の探査機「はやぶさ」によって,世界初の小惑星サンプルリターンも成功し,小惑星の表面物質の分析も進んでいる.このように急速に理解が進む小惑星について,ここでは探査機による探査の視点から紹介する.</p>
書籍等出版物
19講演・口頭発表等
47-
The 56th Lunar and Planetary Science Conference 2025年3月13日
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PERC International symposium on Dust & Parent bodies (IDP2025) 2025年2月27日
担当経験のある科目(授業)
8-
2019年4月 - 現在太陽と太陽系の科学 (放送大学)
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2011年4月 - 現在位置天文学・天体力学 (東京大学)
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2007年4月 - 現在宇宙科学 (玉川大学)
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2006年4月 - 現在宇宙システム工学特論 III (総合研究大学院大学)
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2006年 - 現在宇宙工学概論 (総合研究大学院大学)
共同研究・競争的資金等の研究課題
15-
日本学術振興会 科学研究費助成事業 2023年4月 - 2026年3月
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日本学術振興会 科学研究費助成事業 基盤研究(B) 2018年4月 - 2021年3月
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日本学術振興会 科学研究費助成事業 基盤研究(C) 2016年4月 - 2019年3月
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日本学術振興会 科学研究費助成事業 2003年 - 2006年
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日本学術振興会 科学研究費助成事業 2003年 - 2005年