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Venturi flume

From Wikipedia, the free encyclopedia

In hydrology, a Venturi flume is a device used for measuring the rate of flow of a liquid in situations with large flow rates, such as a river.[1] It is based on the Venturi effect, for which it is named.[2] It was first developed by V.M. Cone in Fort Collins, Colorado.[3]

The Venturi flume consists of a flume with a constricted section in the center. By the Venturi effect, this causes a drop in the fluid pressure at the center of the constriction. By comparing the fluid pressure at the center of the flume with that earlier in the device, the rate of flow can be measured.[4][5]

References

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  1. ^ de Sa, D.O. (2001). Instrumentation Fundamentals for Process Control. Taylor & Francis. p. 9. ISBN 9781560329015. Retrieved 2015-04-21.
  2. ^ Cone, V.M. (23 April 1917). "The Venturi Flume". Journal of Agricultural Research. 9 (4): 115. Retrieved 2 May 2022.
  3. ^ Bennett, Ray S. (March 1972). Cutthroat Flume Discharge Relations (PDF) (Report). Agency for International Development. Retrieved 2 May 2022.
  4. ^ "Venturi flume: Definition from Answers.com". answers.com. Retrieved 2015-04-21.
  5. ^ "Archived copy". Archived from the original on 2008-12-12. Retrieved 2009-06-07.{{cite web}}: CS1 maint: archived copy as title (link)