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Salt Absorption, Not Size, Drives Porous Particle Descent in Stratified Waters

Laboratory experiments validated a new model of how stratified salt diffusion alters porous particle settling.

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Overview

  • The study published in the Proceedings of the National Academy of Sciences reveals that sinking speeds depend on salt uptake relative to particle volume rather than size alone.
  • A theoretical framework integrates drag forces, buoyancy and diffusion-limited salt absorption to predict settling rates of porous particles.
  • Controlled tank experiments with 3D-printed agar particles confirmed that smaller spheres and elongated shapes descend faster than volumetrically equivalent larger particles.
  • Results could refine climate models by improving understanding of ocean nutrient cycling, carbon sequestration and microplastics distribution.
  • Backed by NSF and Office of Naval Research funding, the researchers are now seeking collaborations with oceanographers and climate scientists to explore practical applications.