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Last modified
1/26/2010 10:08:27 AM
Creation date
10/5/2006 4:09:07 AM
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Floodplain Documents
County
Statewide
Basin
Statewide
Title
Steep Channel Water Surface Profiles
Date
7/1/1971
Prepared By
CSU
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />48 <br /> <br />Appendix A <br /> <br />. <br /> <br />USE OF PROGRAM PROFILE <br /> <br />Purpose of Program Profile <br /> <br />The program was written to provide a means of calculating water <br /> <br />surface profiles in natural channels where flow is near critical. <br /> <br />, <br /> <br />Means of data entry is simplified to the maximum extent to allow ease <br /> <br />of comparison for variations of cross-sectional geometries at any <br /> <br />, <br /> <br />given station or set of stations. <br /> <br />Equipment Requirement <br />This program was written F~RTRAN IV for execution on a CDC 6400. <br /> <br />It may be used on other computers with minor ehanges which have an <br /> <br />available storage of 16,000 units. <br /> <br />. <br /> <br />Program Description <br /> <br />Computations are accomplished in two basic parts. The first part <br /> <br />calculates a table of sectional properties at specified water level <br /> <br />increments. The second part then uses these computed sectional prop- <br /> <br />erties to solve for the water surface elevation at the section. The <br /> <br />water surface elevation is computed by an energy balance for subcriti- <br /> <br />cal flows, or from section properties when an energy balance cannot be <br /> <br />attained or computed velocity exceeds twenty feet per second. For <br /> <br />sub critical flows, a computational procedure based on the Standard <br /> <br />Step Method is used. Flows near critical or with a computed velocity <br /> <br />. <br /> <br />greater than allowable are computed by an equation similar to the weir <br /> <br />. <br /> <br />equation, This equation is: <br /> <br />Q = C ARm <br />s <br />
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