ダイヤモンド粉末は地球冷却の地球工学に不適と判明(Diamonds are not a geoengineer’s best friend)

2026-03-23 ワシントン大学セントルイス校

米・Washington University in St. Louisの研究は、地球工学的手法として検討されてきた「ダイヤモンドダストを用いた気候冷却」が現実的でない可能性を示した。ダイヤモンド粒子は太陽光反射能力が高いとされるが、必要量やコストが極めて大きく、実用化は非現実的と評価された。また、大気中での挙動や環境への影響にも不確実性が残る。研究は、気候変動対策としての地球工学技術について、理論的効果だけでなく経済性や実行可能性を総合的に評価する重要性を指摘。より現実的で持続可能な対策の検討が必要と結論づけている。

<関連情報>

ダイヤモンドダスト中のsp2混成炭素不純物による強い光吸収 Strong light absorption by sp2 hybridized carbon impurities in diamond dust

Joshin Kumar, Gwan-Yeong Jung, Taveen S. Kapoor, Rohan Mishra, Rajan K. Chakrabarty
Journal of Aerosol Science  Available online: 24 February 2026
DOI:https://doi.org/10.1016/j.jaerosci.2026.106767

ダイヤモンド粉末は地球冷却の地球工学に不適と判明(Diamonds are not a geoengineer’s best friend)

Highlights

  • Strongly scattering diamond dust is proposed for Solar Radiation Management.
  • Economical detonation synthesis introduces >5% sp2 hybridized carbon impurities.
  • Density Functional Theory revealed a range of highly light-absorbing impurities.
  • Trace impurities on diamond particles introduce shortwave absorption.
  • Impurities decrease diamond’s scattering by up to 25%, questioning its efficacy.

Abstract

Stratospheric aerosol injection (SAI) using diamond dust has been proposed as a solar radiation management (SRM) technique to mitigate global warming by scattering incoming solar radiation, offering advantages over sulfur-based aerosols such as reduced ozone depletion and acid rain risks. However, detonation synthesis—the most economical method for large-scale nanodiamond production—inevitably introduces sp2-hybridized carbonaceous impurities, often forming shells around diamond cores, which may enhance shortwave absorption and undermine SRM efficacy. This study employs density functional theory and ab-initio molecular dynamics to model these impurities across hydrogen-to-carbon (H/C) ratios from 0.0 to 1.0, revealing a continuum of optical properties in which decreasing sp2 content reduces the imaginary refractive index (k). Particle-scale core-shell Mie scattering simulations at 550 nm for diamond cores of 300 nm diameter with carbonaceous impurity shells (1.95 + ki refractive index, shell thickness of ∼0.1–10 nm corresponding to 0.1–10% impurity mass fraction) show that these impurities elevate the effective mass absorption coefficient to up to ∼1 m2/g—nearly 15% that of black carbon (∼7.5 m2/g)—and decrease single-scattering albedo by up to 25% relative to pure diamond. These absorption enhancements, driven by the impurity shell’s k and mass fraction, could shift diamond dust’s radiative forcing toward warming. Our findings highlight the critical need to revisit diamond’s efficacy as an SAI candidate material.

1904環境影響評価
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