Stratified Flow into a Line Sink
Walter R. Debler
Abstract
Walter R. Debler
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.
OpenAlex reports 6 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
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)