Page 388 - Civil Engineering Formulas
P. 388

316                   CHAPTER TWELVE




                                V  2
                                   (1 + K e )
                                 2g
                                                             H

                             Hydraulic
                             grade line









                FIGURE 12.13  With entrance and exit of a culvert submerged, normal pipe
                flow occurs. Discharge is independent of slope. The fluid flows under pres-
                sure. Discharge may be determined from Bernoulli and Manning equations.



             From the Bernoulli equation for the entrance and exit, and the Manning
           equation for friction loss, the following equation is obtained:
                                               2 2
                                       V  2  V n L
                            H   (1   K e )                     (12.69)
                                       2g    2.21R 4/3
           Solution for the velocity of flow yields
                                          H
                          V                                    (12.70)
                                                   4/3
                                            2
                             B(1   K e /2g)   (n L /2.21R )
           where H   elevation difference between headwater and tailwater, ft (m)
                V   velocity in culvert, ft/s (m/s)
                                            2
                                                    2
                 g   acceleration due to gravity, 32.2 ft/s (9.81 m/s )
                K   entrance-loss coefficient
                 e
                 n   Manning’s roughness coefficient
                 L   length of culvert, ft (m)
                R   hydraulic radius of culvert, ft (m)
           The preceding equation can be solved directly because the velocity is the only
           unknown.

           Culverts on Subcritical Slopes
           Critical slope is the slope just sufficient to maintain flow at critical depth.
           When the slope is less than critical, the flow is considered subcritical.
   383   384   385   386   387   388   389   390   391   392   393