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The height limit of a siphon

The maximum height of a siphon is generally assumed to be dependent on barometric pressure—about 10 m at sea level. This limit arises because the pressure in a siphon above the upper reservoir level is below the ambient pressure, and when the height of a siphon approaches 10 m, the pressure at the c...

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Detalles Bibliográficos
Autores principales: Boatwright, A., Hughes, S., Barry, J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4667279/
https://www.ncbi.nlm.nih.gov/pubmed/26628323
http://dx.doi.org/10.1038/srep16790
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author Boatwright, A.
Hughes, S.
Barry, J.
author_facet Boatwright, A.
Hughes, S.
Barry, J.
author_sort Boatwright, A.
collection PubMed
description The maximum height of a siphon is generally assumed to be dependent on barometric pressure—about 10 m at sea level. This limit arises because the pressure in a siphon above the upper reservoir level is below the ambient pressure, and when the height of a siphon approaches 10 m, the pressure at the crown of the siphon falls below the vapour pressure of water causing water to boil breaking the column. After breaking, the columns on either side are supported by differential pressure between ambient and the low-pressure region at the top of the siphon. Here we report an experiment of a siphon operating at sea level at a height of 15 m, well above 10 m. Prior degassing of the water prevented cavitation. This experiment provides conclusive evidence that siphons operate through gravity and molecular cohesion.
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spelling pubmed-46672792015-12-08 The height limit of a siphon Boatwright, A. Hughes, S. Barry, J. Sci Rep Article The maximum height of a siphon is generally assumed to be dependent on barometric pressure—about 10 m at sea level. This limit arises because the pressure in a siphon above the upper reservoir level is below the ambient pressure, and when the height of a siphon approaches 10 m, the pressure at the crown of the siphon falls below the vapour pressure of water causing water to boil breaking the column. After breaking, the columns on either side are supported by differential pressure between ambient and the low-pressure region at the top of the siphon. Here we report an experiment of a siphon operating at sea level at a height of 15 m, well above 10 m. Prior degassing of the water prevented cavitation. This experiment provides conclusive evidence that siphons operate through gravity and molecular cohesion. Nature Publishing Group 2015-12-02 /pmc/articles/PMC4667279/ /pubmed/26628323 http://dx.doi.org/10.1038/srep16790 Text en Copyright © 2015, Macmillan Publishers Limited http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
spellingShingle Article
Boatwright, A.
Hughes, S.
Barry, J.
The height limit of a siphon
title The height limit of a siphon
title_full The height limit of a siphon
title_fullStr The height limit of a siphon
title_full_unstemmed The height limit of a siphon
title_short The height limit of a siphon
title_sort height limit of a siphon
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4667279/
https://www.ncbi.nlm.nih.gov/pubmed/26628323
http://dx.doi.org/10.1038/srep16790
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