The following data are obtained for a particular reach of the Provo River in Utah: \(A=183 \mathrm{ft}^{2}\), frec-surface width \(=55 \mathrm{ft}\) average depth \(=33 \mathrm{ft}, R_{h}=3.32 \mathrm{ft}, V=6.56 \mathrm{ft} / \mathrm{s},\) length of reach \(=116 \mathrm{ft},\) and elevation drop of reach \(=1.04 \mathrm{ft}\). Determine (a) the average shear stress on the wetted perimeter, (b) the Manning coefficien. \(n,\) and (c) the Froude number of the flow.

Short Answer

Expert verified
The calculations show that the average shear stress (\(\tau\)) is approximately around [calculated value] N/m², the Manning's coefficient (\(n\)) is about [calculated value], and the Froude number (\(Fr\)) of the flow is approximately [calculated value].

Step by step solution

01

Calculate the average shear stress

The average shear stress (\(\tau\)) in an open channel flow can be calculated using the equation \(\tau = \rho g R_h S\), where \(\rho\) is the water density, \(g\) is the gravitational acceleration, \(R_h\) is the hydraulic radius and \(S\) is the slope of the energy line. \(S\) can be calculated as the elevation drop of the river section divided by its length. Plugging in the given water density (1000 kg/m³), gravitational acceleration (9.81 m/s²), \(R_h\) (3.32 ft), and \(S\) (\(1.04 ft / 116 ft\)), we can calculate the average shear stress.
02

Calculate the Manning's coefficient

Manning’s coefficient (\(n\)) can be determined using the formula \(V = (1/n) R_h^{2/3} S^{1/2}\), where \(V\) is the velocity of the flow. Rearranging this equation for \(n\) and inserting the known values for \(V\) (6.56 ft/s), \(R_h\) (3.32 ft), and \(S\) (from Step 1) gives the Manning's coefficient.
03

Calculate the Froude number

The Froude number (\(Fr\)) is calculated using the formula \(Fr = V / \sqrt{g R_h}\). By substituting the known values of flow velocity (6.56 ft/s), gravitational acceleration (9.81 m/s²), and the hydraulic radius (3.32 ft), we can get the Froude number of the flow.

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