Flow in partially filled gravity pipe/tunnel

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Flow velocity in a partially filled gravity pipe differs from that in a fully filled pipe due to the presence of a free surface, which affects friction and flow characteristics. The design and gradient of the pipe significantly influence fluid volume and velocity, with variations in topography impacting the system's efficiency. Open channel flow principles apply, highlighting phenomena like surface waves and hydraulic jumps that are not present in fully filled pipes. The Manning equation is commonly used for analyzing such flow scenarios. Understanding these factors is crucial for designing an effective inspection system in a gravity tunnel.
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Hi everybody, I am working on a project to design an inspection system in a gravity tunnel. Can anyone advise me if the flow velocity in a partially filled pipe is the same as the flow velocity in a fully filled pipe?

Thank you in advance!
 
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Can you define what you mean by gravity tunnel? Are you referring to a hypothetical design for an evacuated tunnel through the Earth's mantle to travel between two cities using gravity alone?

https://en.wikipedia.org/wiki/Gravity_train
 
Are you referring to the "gradient" on an ordinary pipe? It will vary depending on the fall of the pipe from start to finish. For example you can generally maintain a downwardly gradient over some distance but depending on the topographical features of where you are going to locate the structure you may have 5 degrees fall in one area in others 3 or less which will affect the volume of fluid the system can handle.
 
kcljk009 said:
Hi everybody, I am working on a project to design an inspection system in a gravity tunnel. Can anyone advise me if the flow velocity in a partially filled pipe is the same as the flow velocity in a fully filled pipe?

Thank you in advance!
What you are looking at is open channel flow, which does have its own pecularities, one of which is the free surface at the top. Friction to flow is along the wetted area, ie the sides and bottom, which as you can now see is the major difference from pipe flow.
Surface waves, hydraulic jumps or drops from changes in gradient are two occurances that one can visually see in particular occurances of channel flow.

The Manning equation is the one equation mostly used for analysis.

Some more info at, which gives some examples,
http://udel.edu/~inamdar/EGTE215/Open_channel.pdf

and at, even if somewhat convoluted,
http://mysite.du.edu/~etuttle/tech/opench.htm
 
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