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Last modified
1/26/2010 10:08:21 AM
Creation date
10/5/2006 4:08:34 AM
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Floodplain Documents
County
Statewide
Basin
Statewide
Title
HEC-2 Water Surface Profiles - Users Manual
Date
11/1/1976
Prepared For
US
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />ApI' \3 = obstructed areas at upstream and downstream sections, <br /> respectively <br />Yl, Y2, Y3 - vertical distance from water surface to center of gravity <br /> of AI' A2' and A3' respectively <br />Ypl' ~2 - vertical distance from water surface to center of gravity <br /> of ApI and Ap3' respectively <br />Q = discharge <br />g - gravitational acceleration <br /> <br />(c) The three parts of the momentum equation represent the total <br />momentum flux in the constriction expressed in terms of the channel properties <br />and flow depths upstream, within and downstream of the constricted section, <br />respectively. If each part of this equation is plotted as a function of the <br />water depth, three curves are obtained, representing the total momentum flux in <br />the constriction for various depths at each location. The desired solutions <br />(water depths) are then readily available for any class of flow. If the water <br />surface profile has been computed to the section at the downstream end of the <br />pier, as is the usual case for subcritical flow, then the downstream depth is <br />known. If the momentum flux for the constriction based on this downstream <br />depth is greater than the momentum flux for the constriction based on critical <br />depth, and the downstream depth is above critical depth, the flow is Class A, <br />and the upstream depth is determined by the use of Yarnell's energy equation <br />since the momentum method does not take into account an exit loss. The depth <br />within the constricted section is determined by solving for the depth of flow <br />which will provide a momentum flux equal to the downstream momentum 'flux. If <br />the downstream momentum flux is less than the momentum flux for the constriction <br />at critical depth, and the downstream depth is above critical, the flow is <br />Class B, and the water surface elevation in the constriction is at critical <br />depth. A new downstream depth (below critical) and the upstream depth (above <br />critical) can be determined by finding the depths whose corresponding momentum <br />fluxes equal the momentum flux at the constriction for critical depth. If <br />the upstream depth is known, as is usually true for supercritical flow, and <br />the momentum flux for the constricted section based on the upstream depth is <br />greater than the momentum flux for the constricted section at critical depth, <br />and the upstream depth is less than critical, the flow is Class C, and the <br />downstream depth and the depth within the bridge section are found by deter- <br />mining depths corresponding to a momentum flux in the constriction based on the <br />upstream depth. If, however, the computed momentum flux for the constricted <br />section based on the upstream depth is less than the momentum flux for the <br />constricted section at critical depth, the flow is Class B and the upstream <br />depth is the depth (above critical) corresponding to the momentum flux for <br />the constricted section at critical depth. The water surface profile must <br /> <br />10 <br />
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