ArticleScientific reports2019
Turbulence mediates marine aggregate formation and destruction in the upper ocean.
Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
5 citing papers in PubMed.
- Modulation of biofilm growth by shear and fluctuations in turbulent environments.Scientific reports · 2025Article
- Persistent reshaping of cohesive sediment towards stable flocs by turbulence.Scientific reports · 2023Article
- A proteome scale study reveals how plastic surfaces and agitation promote protein aggregation.Scientific reports · 2023Article
- In Situ Particle Measurements Deemphasize the Role of Size in Governing the Sinking Velocity of Marine Particles.Geophysical research letters · 2022Article
- Investigation of shear-induced rearrangement of carbon nanotube bundles using Taylor-Couette flow.RSC advances · 2021Article
Corrections and comments
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Authors and funding
6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Marine aggregates formed through particle coagulation, large ones (>0.05 cm) also called marine snow, make a significant contribution to the global carbon flux by sinking from the euphotic zone, impacting the Earth's climate. Since aggregate sinking velocity and carbon content are size-dependent, understanding the physical mechanisms controlling aggregate size distribution is fundamental to determining the biological carbon pump efficiency. Theoretical, laboratory and in-situ studies of flocculation have suggested that turbulence in the benthic boundary layer is important for aggregate formation and destruction, but the small number of field observations has limited our understanding of the role of turbulence on aggregation processes in the ocean surface layer away from energetic boundaries. Using simultaneous field observations of turbulence and aggregates, we show how aggregate formation, destruction, morphology and size distribution in the ocean surface layer (10-100 m) are mediated by interactions between turbulence and aggregate concentration. Our findings suggest that turbulence enhances aggregate formation up to a critical turbulent kinetic energy dissipation rate of 10
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Registered trials
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