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Plumes of settling and dissolving sugar grains.

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Bibliographic Details
Title:	Plumes of settling and dissolving sugar grains.
Authors:	Kriaa, Quentin^1,2,3 (AUTHOR) qk207@cam.ac.uk, Favier, Benjamin^1,2 (AUTHOR), Le Bars, Michael^1,3 (AUTHOR)
Source:	Journal of Fluid Mechanics. 11/10/2025, Vol. 1022, p1-37. 37p.
Subjects:	Fluid dynamics, Plumes (Fluid dynamics), Sugar, Precipitation (Chemistry), Dissolution (Chemistry), Rayleigh-Taylor instability, Laminar flow, Particle image velocimetry
Abstract:	We present experiments of settling and dissolving sugar grains continuously sieved above a water tank with varying grain size and mass flux. Through drag and dissolution, grains force a downward flow whose dynamics are analysed in a laser sheet through particle image velocimetry and the use of home-made fluorescent sugar to track the negatively buoyant sugary water. We reveal different regimes, mostly controlled by the grain size, from a particle-constrained laminar flow at large grain size, to a turbulent plume with an effectively fluid-like behaviour when grains are small. The transitions between regimes are predicted from dimensionless numbers quantifying fluid–particle coupling, collective effects between grains and the possible onset of a Rayleigh–Taylor instability at the source. When a quasi-steady regime is reached, all grains dissolve above a finite depth, below which the flow is exclusively driven by dissolved sugar. We derive simple idealised models based on the source properties that predict the depth of this dissolution layer as well as the characteristic flow velocity. [ABSTRACT FROM AUTHOR]
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Database:	Engineering Source

Description
Abstract:	We present experiments of settling and dissolving sugar grains continuously sieved above a water tank with varying grain size and mass flux. Through drag and dissolution, grains force a downward flow whose dynamics are analysed in a laser sheet through particle image velocimetry and the use of home-made fluorescent sugar to track the negatively buoyant sugary water. We reveal different regimes, mostly controlled by the grain size, from a particle-constrained laminar flow at large grain size, to a turbulent plume with an effectively fluid-like behaviour when grains are small. The transitions between regimes are predicted from dimensionless numbers quantifying fluid–particle coupling, collective effects between grains and the possible onset of a Rayleigh–Taylor instability at the source. When a quasi-steady regime is reached, all grains dissolve above a finite depth, below which the flow is exclusively driven by dissolved sugar. We derive simple idealised models based on the source properties that predict the depth of this dissolution layer as well as the characteristic flow velocity. [ABSTRACT FROM AUTHOR]
ISSN:	00221120
DOI:	10.1017/jfm.2025.10766