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Journal ArticleDOI

The onset of cellular convection in a fluid layer with time-dependent density gradients

TLDR
Onset times for convection induced by buoyancy forces have been measured in three aqueous systems in terms of a critical value for a time-dependent Rayleigh number as mentioned in this paper.
Abstract
Onset times for convection induced by buoyancy forces have been measured. Results on three aqueous systems are summarized in terms of a critical value for a time-dependent Rayleigh number. Because of the presence of minute traces of unavoidable surface-active contaminants, a ‘free’ water surface behaved as if it were inflexible and laterally rigid so far as determining first convective motion was concerned. The form of the onset motion was observed with schlieren photography for both top and side view. The pattern at onset was frequently in the form of plunging rings. Surface effects were demonstrated with an organic liquid layer in which onset times were measured for convection driven by surface tension gradients as well as by buoyancy forces. The data are compared with some recent predictions of linear stability analyses.

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Citations
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Transient high-Rayleigh-number thermal convection with large viscosity variations

TL;DR: In this article, the authors studied the characteristics of thermal convection in a fluid whose viscosity varies strongly with temperature and showed that the upper boundary of an isothermal layer of Golden Syrup is cooled rapidly and maintained at a fixed temperature.
Journal ArticleDOI

Onset of thermal convection in fluids with temperature‐dependent viscosity: Application to the oceanic mantle

TL;DR: In this paper, the authors reevaluate the hypothesis of small-scale convection beneath the oceanic lithosphere with laboratory experiments in fluids whose viscosity depends strongly on temperature and derive scaling laws for the onset time and for the surface heat flow.
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Physics of multiscale convection in Earth's mantle: Evolution of sublithospheric convection

TL;DR: In this article, scaling laws for the breakdown of layered convection as well as the strength of convection are derived as a function of viscosity layering, the phase buoyancy parameter, and the thermal Rayleigh number.
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Mantle mixing and continental breakup magmatism

TL;DR: In this article, the authors demonstrate that sublithospheric convection driven by surface cooling can bring up dense fertile mantle without a thermal anomaly, and this multi-scale mantle mixing could potentially explain a variety of hotspot phenomenology as well as the formation of both volcanic and non-volcanic rifted margins.
References
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Journal ArticleDOI

On cellular convection driven by surface-tension gradients: effects of mean surface tension and surface viscosity

TL;DR: In this article, the onset of steady, cellular convection driven by surface tension gradients on a thin layer of liquid is examined in an extension of Pearson's (1958) stability analysis.
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Surface tension and buoyancy effects in cellular convection

TL;DR: In this article, a Fourier series method has been used to obtain the eigenvalue equation for the case where the lower boundary surface is a rigid conductor and the upper free surface is subject to a general thermal condition.
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Stability of a Homogeneous Fluid Cooled Uniformly from Above

TL;DR: In this article, the stability of an initially homogeneous layer of fluid which is cooled uniformly from above is examined, and a simplified mathematical model in which the velocity and temperature perturbations vanish at the top and bottom boundaries but which takes into account nonlinear, time-dependent temperature profiles is developed.
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Convective Circulation in Water Induced by Evaporative Cooling

TL;DR: Schlieren photographs taken simultaneously from the top and side of a tank of water are used to study convection currents induced by evaporative cooling as discussed by the authors, and it is found that water from the cooled surface layer collects along lines producing thickened regions which become unstable and plunge in vertical sheets.
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The effect of surface active agents on convection cells induced by surface tension

TL;DR: In this article, the stabilization of convection induced by surface tension is predicted theoretically by extending P earson's stability analysis of surface tension induced convection to account for the presence of surface active agents.
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