Appendix 9.2. Hydraulics Of Open Channel Flow  


§ 9.2.1. Energy
§ 9.2.2. Specific Energy
Appendix 9.2.3. Flow Classification
§ 9.2.3.1. Types of Flow in Open Channels
§ 9.2.3.2. Critical Flow
§ 9.2.3.3. Subcritical Flow
§ 9.2.3.4. Supercritical Flow
Appendix 9.2.4. Uniform Flow
§ 9.2.4.1. Manning's Equation
§ 9.2.5. Gradually Varied Flow
§ 9.2.6. Rapidly Varied Flow
Appendix 9.2.7. Hydraulic Jump
§ 9.2.7.2. Types of Hydraulic Jump
§ 9.2.7.3. Hydraulic Jump in Horizontal Channels

Hydraulic calculations shall be performed by using the U.S. Army Corps of Engineers HEC-RAS "River Analysis System" computer models. Normal depth channel calculations are permissible for constructed open channels with a uniform geometric cross section where 1) there is no potential for the water surface elevations to be controlled by backwater and 2) the channel is not in a FEMA floodplain.

Certain watersheds have hydrologic and hydraulic models that are available through the San Antonio River Authority website, Digital Data & Modeling Repository (D2MR). Developments proposed within the limits of these watersheds must have the models updated by the design engineer to reflect changes in flow, channel configuration (including alterations to vegetation) and channel structures. The design engineer's models must use the same computer program that was used in the existing model e.g. HEC-RAS or FEMA latest accepted models. The updated models shall be submitted to the Director of TCI.

The influence of gravity on fluid motion in an open channel flow can be expressed in a dimensionless quantity called a Froude Number (Fr). The Froude Number is expressed in the following equation.

(Equation 9.2)

35-H9-2.png

V = Mean velocity (fps)
g = Acceleration of gravity = 32.2 ft/s
d = Hydraulic depth (ft.)

The hydraulic depth is defined as the cross sectional area of the channel perpendicular to the flow divided by the free water surface.