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Journal ArticleDOI

Forced plumes and mixing of liquids in tanks

A. E. Germeles
- 14 Oct 1975 - 
- Vol. 71, Iss: 03, pp 601-623
TLDR
In this paper, the mixing of two miscible liquids of slightly different densities was considered, where one of them (cargo) was injected into a tank partially filled with the other (inventory), such that buoyancy and inertia act in concert on the plume produced by the cargo.
Abstract
We consider the mixing between two miscible liquids of slightly different density (< 10%) when one of them (cargo) is injected into a tank partially filled with the other (inventory). The injection of the cargo is such that buoyancy and inertia act in concert on the plume produced by the cargo. The two basic processes that govern the mixing of the two liquids in the tank are the entrainment of tank liquid by the plume and the tank circulation set up by this entrainment and by the plume discharge. Unlike plumes in an environment of infinite extent, the plume in this case changes its environment continuously, which, in turn, has a continuously-varying effect on the plume. A mathematical model for the mixing of the two liquids is presented, from which one can compute the tank stratification that may result when given amounts of cargo and inventory are thus mixed. Plume entrainment theory is used for the plume dynamics and a ‘filling-box’ model is used for the tank circulation. The partial differential equations of the model are integrated by an original and unique numerical method. The problem was also treated experimentally. The tank stratification is expressed in terms of a normalized density-difference variable δ. Except for some very localized large discrepancies, due to certain local effects not included in the model, computed and experimental profiles of δ agree very well, their maximum and average deviations being within 4 and 2%, respectively. It is found that values of the empirical plume parameters α and λ that are used commonly for steady plumes in environments of infinite extent are approximately right for the time-dependent plumes under consideration too.

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Citations
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Convection and mixing in magma chambers

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Turbulent buoyant convection from a source in a confined region

TL;DR: In this paper, an extension of the model first proposed by Baines & Turner (1969) is derived with careful attention to the conditions required for its application, such as the Prandtl number ν/k is of order unity or greater, the ratio of the length L to depth H of the region is greater than about 1·2 for the two-dimensional region considered and R is so large that R [gsim ] L/H and R [Gt ] 1/α.
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Significance of 87 Sr/ 86 Sr ratios in the Merensky cyclic unit of the Bushveld Complex

TL;DR: In this paper, the results of a detailed Sr-isotope study across the Merensky unit and its immediate foot-and hangingwall-rocks are presented, when considered together with new ideas on processes operating in magma chambers.
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Time-dependent density profiles in a filling box

TL;DR: In this paper, an approximate analytic expression for the time-dependent density profile formed by a turbulent buoyant plume in a confined region is presented based on the approximation that the density of the fluid behind the first front changes at a rate which is virtually independent of position.
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Convective fractionation: A mechanism to provide cryptic zoning (macrosegregation), layering, crescumulates, banded tuffs and explosive volcanism in igneous processes

TL;DR: In this article, a large array of igneous and volcanic features has been recognized as conclusive and direct evidence of convection in stratified and/or solidifying melts; e.g., macroscopic segregation (cryptic variation, zoning in magma chambers), mineral layering (in mafic intrusives), crescumulates (fingering) in the vertical and horizontal, banding (in pyroclastics), rollover with attendant flashing of volatiles (explosive volcanism), etc.
References
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Book

Buoyancy Effects in Fluids

J. S. Turner
TL;DR: In this article, the authors introduce linear internal waves and herar flows in a stratified fluid and double-diffusive convection in stably stratified fluids, and show that the shear flows can produce turbulence.
Journal ArticleDOI

Turbulent gravitational convection from maintained and instantaneous sources

TL;DR: In this article, the authors developed a theory of convection from maintained and instantaneous sources of buoyancy, using methods which are applicable to stratified body fluids with any variation of density with height; detailed solutions have been presented for the case of a stably stratified fluid with a linear density gradient.
Journal ArticleDOI

Turbulent buoyant convection from a source in a confined region

TL;DR: In this article, the effect of continuous convection from small sources of buoyancy on the properties of the environment when the region of interest is bounded is considered, assuming that the entrainment into the turbulent buoyant region is at a rate proportional to the local mean upward velocity, and that the buoyant elements spread out at the top of the region and become part of the non-turbulent environment at that level.
Journal ArticleDOI

Gravitational Convection from a Boundary Source

TL;DR: In this paper, the mean patterns of free convection from a line source and a point source are presented without regard to the specific means by which the gravitational action is produced, and derived functional relationships are then verified and completed through use of velocity and temperature measurements above sources of heat, the generalized form of the results permitting characteristics of the mean flow to be determined over a considerable range of primary variables.
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