Self-similar gravity currents with variable inflow revisited: Plane currents

We use shallow-water theory to study the self-similar gravity currents that describe the intrusion of a heavy fluid below a lighter ambient fluid. We consider in detail the case of currents with planar symmetry produced by a source with variable inflow, such that the volume of the intruding fluid va...

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Autores principales: Gratton, J., Vigo, C.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00221120_v258_n_p77_Gratton
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spelling todo:paper_00221120_v258_n_p77_Gratton2023-10-03T14:26:33Z Self-similar gravity currents with variable inflow revisited: Plane currents Gratton, J. Vigo, C. Boundary value problems Density (specific gravity) Gravity waves Hydraulic jump Froude number Power law Self similar gravity currents Shallow water theory Supercritical subcritical transition Variable inflow Flow interactions Currents Gravity Flow Inflow density flow plane currents shallow-water theory We use shallow-water theory to study the self-similar gravity currents that describe the intrusion of a heavy fluid below a lighter ambient fluid. We consider in detail the case of currents with planar symmetry produced by a source with variable inflow, such that the volume of the intruding fluid varies in time according to a power law of the type f. The resistance of the ambient fluid is taken into account by a boundary condition of the von Karman type, that depends on a parameter β that is a function of the density ratio of the fluids. The flow is characterized by β, α, and the Froude number F0 near the source. We find four kinds of self-similar solutions: subcritical continuous solutions (Type I), continuous solutions with a supercritical-subcritical transition (Type II), discontinuous solutions (Type III) that have a hydraulic jump, and discontinuous solutions having hydraulic jumps and a subcritical-supercritical transition (Type IV). The current is always subcritical near the front, but near the source it is subcritical (F0 < 1) for Type I currents, and supercritical (F0 > 1) for Types II, III, and IV. Type I solutions have already been found by other authors, but Type II, III, and IV currents are novel. We find the intervals of parameters for which these solutions exist, and discuss their properties. For constant-volume currents one obtains Type I solutions for any β that, when β > 2, have a ‘dry’ region near the origin. For steady inflow one finds Type I currents for 0 < β < ∞ and Type II and III currents for any 8, if is sufficiently large. © 1994, Cambridge University Press. All rights reserved. Fil:Gratton, J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vigo, C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00221120_v258_n_p77_Gratton
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Boundary value problems
Density (specific gravity)
Gravity waves
Hydraulic jump
Froude number
Power law
Self similar gravity currents
Shallow water theory
Supercritical subcritical transition
Variable inflow
Flow interactions
Currents
Gravity Flow
Inflow
density flow
plane currents
shallow-water theory
spellingShingle Boundary value problems
Density (specific gravity)
Gravity waves
Hydraulic jump
Froude number
Power law
Self similar gravity currents
Shallow water theory
Supercritical subcritical transition
Variable inflow
Flow interactions
Currents
Gravity Flow
Inflow
density flow
plane currents
shallow-water theory
Gratton, J.
Vigo, C.
Self-similar gravity currents with variable inflow revisited: Plane currents
topic_facet Boundary value problems
Density (specific gravity)
Gravity waves
Hydraulic jump
Froude number
Power law
Self similar gravity currents
Shallow water theory
Supercritical subcritical transition
Variable inflow
Flow interactions
Currents
Gravity Flow
Inflow
density flow
plane currents
shallow-water theory
description We use shallow-water theory to study the self-similar gravity currents that describe the intrusion of a heavy fluid below a lighter ambient fluid. We consider in detail the case of currents with planar symmetry produced by a source with variable inflow, such that the volume of the intruding fluid varies in time according to a power law of the type f. The resistance of the ambient fluid is taken into account by a boundary condition of the von Karman type, that depends on a parameter β that is a function of the density ratio of the fluids. The flow is characterized by β, α, and the Froude number F0 near the source. We find four kinds of self-similar solutions: subcritical continuous solutions (Type I), continuous solutions with a supercritical-subcritical transition (Type II), discontinuous solutions (Type III) that have a hydraulic jump, and discontinuous solutions having hydraulic jumps and a subcritical-supercritical transition (Type IV). The current is always subcritical near the front, but near the source it is subcritical (F0 < 1) for Type I currents, and supercritical (F0 > 1) for Types II, III, and IV. Type I solutions have already been found by other authors, but Type II, III, and IV currents are novel. We find the intervals of parameters for which these solutions exist, and discuss their properties. For constant-volume currents one obtains Type I solutions for any β that, when β > 2, have a ‘dry’ region near the origin. For steady inflow one finds Type I currents for 0 < β < ∞ and Type II and III currents for any 8, if is sufficiently large. © 1994, Cambridge University Press. All rights reserved.
format JOUR
author Gratton, J.
Vigo, C.
author_facet Gratton, J.
Vigo, C.
author_sort Gratton, J.
title Self-similar gravity currents with variable inflow revisited: Plane currents
title_short Self-similar gravity currents with variable inflow revisited: Plane currents
title_full Self-similar gravity currents with variable inflow revisited: Plane currents
title_fullStr Self-similar gravity currents with variable inflow revisited: Plane currents
title_full_unstemmed Self-similar gravity currents with variable inflow revisited: Plane currents
title_sort self-similar gravity currents with variable inflow revisited: plane currents
url http://hdl.handle.net/20.500.12110/paper_00221120_v258_n_p77_Gratton
work_keys_str_mv AT grattonj selfsimilargravitycurrentswithvariableinflowrevisitedplanecurrents
AT vigoc selfsimilargravitycurrentswithvariableinflowrevisitedplanecurrents
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