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FLOOD09845
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Last modified
1/26/2010 10:10:48 AM
Creation date
10/5/2006 4:41:17 AM
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Floodplain Documents
County
Statewide
Community
State of Colorado
Basin
Statewide
Title
Floodplain Management Workshop
Date
2/10/1993
Prepared For
Greeley
Prepared By
CWCB
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />Substituting (2) into (I) we obtain: <br /> <br />Q = 1.486(1)- ) [k]~ sj <br />n y b+2y , <br /> <br />(3) <br /> <br />To isolate b or y in this equation so it can be solvable quickly becomes a mathematical nightmare, The <br />math only gets worse if the channel is trapezoidal, circular, triangulay, or other commonly used shapes, To <br />help alleviate the headaches of solving equations manually every time one wishes to size a hydranlic struc- <br />ture, various tables, nomographs and charts have been developed for design aids, Several of these aids are <br />included in this handout and shonld prove useful. <br /> <br />1. OPEN CHANNELS <br /> <br />An open channel can be of nearly any configuration desired, however the most commonly used design falls <br />into the trapezoidal category, In this case we will dwell on Olis type of open channel. <br /> <br />Table 2 presents values of K which can be used to detemliue the rEquired bottom width of a trapezoidal <br />channel with identical bank slopes, Substituting the parameters of a trapezoidal channel into equation (I) <br />and breaking it down into a usable form results in equation (4); <br /> <br />2 I <br />QK,S' <br />=; y 0 <br /> <br />(4) <br /> <br />K is a catch-all variable that encompasses the parameters of the channel. For this instance, K is identified <br />by the equation; <br /> <br />K= <br /> <br />[ IJ ~13 <br />1.486 z + ~ <br /> <br />[I ] 2'3 <br />~+ 2V(z2 + I) , <br /> <br />(5) <br /> <br />In equation (5), z is the channel sideslope, ely, and x h; the (kpth:width ratio, ylb, <br /> <br />Solving equation (4) for K: <br /> <br />-~ <br />K- &'3S1n <br />y , <br /> <br />(6) <br /> <br />Knowing the parameters for the right side of equation (6), you can solve for K and find the corresponding <br />bottom width of the channel utilizing tablll I. For example, a flow of 80 cfs in a grass lined channel with <br />equal 3;1 side slopes, n = 0.028, desired depth of flow y = 2 ft., and the slope S, =, 0,0042 ft/ft: <br /> <br />80.0.028 <br />K = 2&'30.0042In = 5.443 <br /> <br />Look in table I in the column headed 3 for a 3:1 side slope and locate 5.443, The number falls between <br />5.401 and 5,461. Moving to the left of the table we find Ole corresponding ylb values of 0.47 and 0.48, <br />Interpolating between these values yields a ylb value of 0.477, Now solve for b: <br /> <br />Pag~ 4 <br />(,reenhonu & O'Mora, lnc. <br />
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