小惑星探査機OSIRIS-RExのサンプルに驚くべきリン酸塩の発見(Surprising Phosphate Finding in NASA’s OSIRIS-REx Asteroid Sample)

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2026-06-26 NASA

小惑星探査機OSIRIS-RExのサンプルに驚くべきリン酸塩の発見(Surprising Phosphate Finding in NASA’s OSIRIS-REx Asteroid Sample)

NASAのOSIRIS-RExミッションによって回収された小惑星ベンヌのサンプルの初期分析で、炭素、窒素、有機化合物に富んだ塵が発見されました。これらは生命の必須成分です。主に蛇紋石を含む粘土鉱物で構成され、地球の中央海嶺の岩石に類似しています。サンプルには予想外に純粋なマグネシウム-ナトリウムリン酸塩が含まれ、小惑星が古代の小さな原始的な海洋世界から分裂した可能性を示唆しています。この発見は、ベンヌの歴史的条件に関する貴重な手がかりを提供します。科学者たちは、このサンプルが太陽系の初期と地球上の生命の起源に関する秘密を解明する鍵となると期待しています。

<関連情報>

実験室での小惑星(101955)ベンヌ: OSIRIS-RExが採取したサンプルの特性 Asteroid (101955) Bennu in the laboratory: Properties of the sample collected by OSIRIS-REx

Dante S. Lauretta, Harold C. Connolly Jr, Joseph E. Aebersold, Conel M. O’D. Alexander, Ronald-L. Ballouz, Jessica J. Barnes, Helena C. Bates, Carina A. Bennett, Laurinne Blanche …
Meteoritics & Planetary Science  Published: 26 June 2024
DOI:https://doi.org/10.1111/maps.14227

Abstract

On September 24, 2023, NASA’s OSIRIS-REx mission dropped a capsule to Earth containing ~120 g of pristine carbonaceous regolith from Bennu. We describe the delivery and initial allocation of this asteroid sample and introduce its bulk physical, chemical, and mineralogical properties from early analyses. The regolith is very dark overall, with higher-reflectance inclusions and particles interspersed. Particle sizes range from submicron dust to a stone ~3.5 cm long. Millimeter-scale and larger stones typically have hummocky or angular morphologies. Some stones appear mottled by brighter material that occurs as veins and crusts. Hummocky stones have the lowest densities and mottled stones have the highest. Remote sensing of Bennu’s surface detected hydrated phyllosilicates, magnetite, organic compounds, carbonates, and scarce anhydrous silicates, all of which the sample confirms. We also find sulfides, presolar grains, and, less expectedly, Mg,Na-rich phosphates, as well as other trace phases. The sample’s composition and mineralogy indicate substantial aqueous alteration and resemble those of Ryugu and the most chemically primitive, low-petrologic-type carbonaceous chondrites. Nevertheless, we find distinct hydrogen, nitrogen, and oxygen isotopic compositions, and some of the material we analyzed is enriched in fluid-mobile elements. Our findings underscore the value of sample return—especially for low-density material that may not readily survive atmospheric entry—and lay the groundwork for more comprehensive analyses.

1701物理及び化学
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