雨滴衝突直後に発生する新たな土壌侵食メカニズムを解明(A physicist who also grows trees investigates the fate of raindrops)

2026-02-17 スイス連邦工科大学ローザンヌ校(EPFL)

スイス連邦工科大学ローザンヌ校の物理学者ベルティル・トロテ氏は、家族経営の果樹園を営む傍ら、雨滴による新たな土壌侵食機構を解明した。共同研究(米ペンシルベニア大学と実施、PNAS掲載)では、乾燥した傾斜地で雨滴が跳ねた後に転がり、砂粒を取り込んで「サンドボール」に成長し、衝突時の最大約10倍の土壌を移動させ得ることを示した。形状はピーナツ型とドーナツ型の2種。実験室と野外観測で確認され、乾燥・山地環境での侵食評価の見直しや、肥料・食品粒子の低摩擦製造への応用可能性も示唆した。

<関連情報>

雨滴から砂玉が生まれる Sandball genesis from raindrops

Bertil Trottet, Daisuke Noto, Douglas J. Jerolmack, and Hugo N. Ulloa
Proceedings of the National Academy of Sciences  Published:December 22, 2025
DOI:https://doi.org/10.1073/pnas.2519392122

Significance

Raindrops do not just splash—they can roll, gather, and grow. While erosion is often thought to begin and end the moment a raindrop hits the ground, we found that the story continues: On sloped, dry soil, raindrops can roll downhill like tiny snowballs, picking up grains along the way and forming what we call “sandballs.” This process greatly amplifies the amount of soil a single drop can move—by up to ten times—revealing a powerful and previously overlooked erosion mechanism. Understanding how water and soil interact at this scale can help improve models of landscape change, soil loss, and agriculture. It may also inspire innovations in fields like bioengineering, food processing, and snow and soft matter physics.

Abstract

In the water cycle, erosion begins with the entrainment of soil by raindrops. The discrete, discontinuous, and three-phase nature of raindrop erosion—at the boundary of fluid and granular mechanics—makes this problem particularly challenging, compared to better-studied sediment transport by river and wind currents. Past research has emphasized particle entrainment by raindrop splash at impact. Here, we report lab and field observations, that uncover a surprisingly rich and efficient postimpact phase. Raindrops impacting a dry, sloping, granular bed spontaneously form “sandballs;” drops of dense suspensions that can grow in mass to a jammed state by sediment entrainment, as they roll downhill like snowballs and magnify soil erosion. Careful control of drop conditions reveals two stable sandball morphologies: peanut-like shapes linked to hydrodynamic instabilities and toroidal forms that undergo mechanical locking from extreme sediment loading, which have potential implications for related problems in bioengineering, pharmaceuticals, and snow physics.

1702地球物理及び地球化学
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