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Drainage Trench Conveyance Capacity

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waterboy123

Civil/Environmental
Oct 24, 2012
6
Hello,

If I have a drainage trench 600mm x 600mm filled with large stones, assuming a porosity of 0.33 and a gradient of 1/200 what is the best way to caculate the conveyance capacity in l/s. In other words what is the maximum flow rate the trench can pass downstream to the outfall.

I would assume using mannings formula with a very high n value wouldn't be suitable?

Thanks
 
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Internet search "riprap intersitial flow". You'll find several references. However, at that shallow gradient, the discharge will be very small.
 
Is it lined, or filled all the way up? For a riprap liner, use Manning's. For it completely full, you're into more complex territory.

Hydrology, Drainage Analysis, Flood Studies, and Complex Stormwater Litigation for Atlanta and the South East -
 
Look into Darcy's equation for sub surface flow. You'll have to come up with the hydraulic conductivity for your specific stone size, gradation and porosity.
 
Thanks for the responses. Just to confirm the trench will be filled all the way to the top with stone and lined with a membrane to stop soil ingress. I was hoping I could just use mannings and divide the answer by 3 (the stone creates 33% free space within the trench). I thought it might be Darcy's equation but that might be more complex than I wanted to go :-(
 
Please see attachment. The problem with Darcy is I have no way of accessing the delta H, ie the change in water level across the trench. If I new this I could calculate Q and everything would be good in the world.
 
 http://files.engineering.com/getfile.aspx?folder=422d5081-25b8-4775-af02-cb21776e84e1&file=trench_conveyance.pdf
It's a differential equation where i = dh/dx:

Q=K(dh/dx)By
and, y = h - Sx
or Q = K (dh/dx)B(h - Sx)

B = Width
y = Depth
x = location upstream from the downstream end
S = bottom slope
h = energy head (y + Sx)

The differential equation can be solved using a standard step method, and by varing Q until h = the top of the channel at the upstream end.

 
you cannot solve this with any degree of accuracy given the data you have and Mannings equation is completely out of the question. stick with darcy. a reasonable estimate might be to assume an avg cross sectional area and delta h. solve for a range of hydraulic conductivities to give an estimate of the range of possible flows.
 
No! Manning's is not to be applied to interstitial rock flow! Totally inappropriate!
 
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