1961•Transactions of the American Society of Civil EngineersRequires access

Stratified Flow into a Line Sink

Walter R. Debler

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Abstract

The discharge of a stratified fluid (with a stable linear density variation at infinity) through a horizontal slot at the end of a channel has been experimentally investigated. The experiments show that when the densimetric Froude number is less than 0.28, the flow pattern is divided into two horizontal regions; an upper, essentially a stagnant region, and a lower region in which the entire discharge is concentrated. The specific results obtained are useful for the solution of many engineering problems involving stratified flows.

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What this paper is about

The discharge of a stratified fluid (with a stable linear density variation at infinity) through a horizontal slot at the end of a channel has been experimentally investigated. The experiments show that when the densimetric Froude number is less than 0.28, the flow pattern is divided into two horizontal regions; an upper, essentially a stagnant region, and a lower region in which the entire discharge is concentrated. The specific results obtained are useful for the solution of many engineering problems involving stratified flows.

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Available abstract

The discharge of a stratified fluid (with a stable linear density variation at infinity) through a horizontal slot at the end of a channel has been experimentally investigated. The experiments show that when the densimetric Froude number is less than 0.28, the flow pattern is divided into two horizontal regions; an upper, essentially a stagnant region, and a lower region in which the entire discharge is concentrated. The specific results obtained are useful for the solution of many engineering problems involving stratified flows.

Key concepts: Froude number, Stratified flow, Stratified flows, Mechanics, Sink (geography), Geology, Flow (mathematics), Line (geometry)

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