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Last modified
1/25/2010 6:27:01 PM
Creation date
10/4/2006 11:40:45 PM
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Title
Engineering and Design Hydraulic Design of Flood Control Channels
Date
7/1/1991
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />EM 1110-2-1601 <br />1 Jul 91 <br /> <br />b, Friction losses, <br /> <br />(1) The importance that friction plays in the determi- <br />nation cf flow characteristics in channels cannot be over- <br />stressed. Three equations (Chezy's. Manning's. and <br />Darcy's) are in genetal use for the determination of losses <br />due to friction. These equations expressed as friction <br />slope Sf. i.e.. slope of the energy grade line. are <br /> <br />(a) Chezy: <br /> <br />S . v2 <br />f - <br />COR <br /> <br />(2-1) <br /> <br />(b) Manning: <br /> <br />V2n2 <br />Sf . <br />2.21R4/~ <br /> <br />(2-2) <br /> <br />(c) Darcy: <br /> <br />S . fV2 <br />f m<g <br /> <br />(2-3) <br /> <br />where <br /> <br />v = velocity <br /> <br />C = Chezy coefficient <br /> <br />f = Darcy-Weisbach resistance <br />coefficient <br /> <br />g = acceleration of gravity <br /> <br />The relation between the coefficients in these equations <br />can be expressed as <br /> <br />C . Rl/6 . 10.8 <br />.l.. 4l:lb n-- fIn" <br /> <br />(2-4) <br /> <br />(2) When determining friction coefficients. it should <br />be recognized that the energy grade line and therefore the <br />friction coefficient include uniformly occumng turbulence <br />and eddy losses as well as the friction loss. Equivalent <br /> <br />2-2 <br /> <br />roughness for the s:une reason. Special. locally occurring <br />turbulence and eddy losses are to be determined sepa- <br />rately as covered in hydr:wlic textbooks and elsewhere in <br />this manual. <br /> <br />c. Friction coefficients, <br /> <br />(1) The equations for using equivalent roughness to <br />determine friction coefficients (plate 3) are <br /> <br />(a) For hydraulically smooth channels <br /> <br />(5.2Rn) <br />C . 32.6 loglO t ~ <br /> <br />(2-5) <br /> <br />(b) For hydraulically rough channels <br /> <br />C. 32.6 loglO (12/R) <br /> <br />(2-6) <br /> <br />where R" is the Reynolds number. <br /> <br />(2) For the channel surlace to be hydraulically <br />smooth. the equivalent roughness must be less than the <br />critical value given by paragraph 8-12 of Chow (1959). <br /> <br />kc . (* )(~) <br /> <br />(2-7) <br /> <br />where v is the kinematic viscosity of water. <br /> <br />(3) Most channels (including concrete.lined chan- <br />nels) with appreciable velocity are hydraulically rough. <br />Plates 4 and 5 are furnished as an aid for determining <br />friction coefficients from equivalent roughness. Irrigation <br />and power canals generally fall in the transition zone <br />shown in Plate 3. <br /> <br />(4) Table 2-1. extracted from HDC sheets 631 to <br />631-2, provides accepClble equivalent roughness values <br />for SlI3ight. concrete,lined channels. <br /> <br />(5) See Chapter 3 for friction coefflcients for riprap. <br /> <br />(6) Values of k for natural river channels usually <br />fall between 0.1 and 3,0 ft (see Table 8-1 of Chow <br />
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