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Last modified
11/23/2009 10:40:01 AM
Creation date
10/4/2006 9:58:59 PM
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Title
Guide for Selecting Roughness Coefficient n Values for Stream Channels
Date
12/1/1963
Prepared By
USDA Soil Conservation Service
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />B.2 <br /> <br />IIIIIIIIIIII Selection of basic n value. This step requires the selec- <br />tion~ n value for a straight, uniform, smooth channel in the <br />natural materials involved, The selection involves consideration of what <br />may be regarded as a hypothetical channel. The conditions of straight <br />alignment, uniform cross section, and smooth side ,and bottom surfaces with- <br />out vegetation should be kept in mind, Thus the basic n will be visualized <br />as varying only with the materials forming the sides and bottom of the <br />channel. The minimum values of n shown by reported test results for the <br />. best channels in earth are in the range from 0.016 to 0.018. Practical <br />limitations associated with maintaining smooth and uniform channels in <br />earth for' any appreciable period indicate that 0,02 is a realistic basic n. <br />The .basic n, as it is intended for use in this procedure, for natural or <br />excavated channels, ~y be selected from the table below. Where the oottom' <br />.and sides of a channel are of different materials this fact may be recog- <br />nized in' selecting the basic n, <br /> <br />Character of channel <br /> <br />Basic n <br /> <br />Channels in earth <br />Channels cut into rock <br />Channels in fine gravel <br />Channels in coarse gravel <br /> <br />0,02 <br />0.025 <br />0.024 <br />0,028 <br /> <br />__election of modifying value for surface irregularity. The <br />sel~e based on the degree of roughness or irregularity of the <br />surfaces of channel sides and bottom. Consider the actual surface irregulari- <br />ty; first} in relation to the degree of surface smoothness obtainable with <br />the natural materials involved, and second, in relation to the depths of flow <br />under. consideration. Actual surface irregularity comparable to the best sur- <br />face to be expected of the natural materials involved c~s for a modifying <br />value of zero. Higher degrees of irregularity. induce turbulence and call for <br />increased modifying values, The table below may be used as a guide to the <br />sel.ection. <br /> <br />DeRree of irreRUlarity <br />Smooth <br /> <br />Surfaces comparable to <br /> <br />The best obtainable for the <br />materials involved, <br /> <br />ModifyinR value <br /> <br />0,000 <br /> <br />Minor <br /> <br />Good dredged channels; slightly <br />eroded or scoured side slopes <br />of canals or drainage channels, 0.005 <br /> <br />Moderate <br /> <br />Fair to poor dredged channels; <br />moderately sloughed or eroded side <br />slopes of canals or drainage <br />channels. 0,010 <br /> <br />Severe <br /> <br />Badly sloughed banks of natural <br />channels; badly eroded or sloughed <br />sides of canals or drainage channels; <br />unshaped, jagged and irregular sur- <br />faces of channels excavated in <br />rock. 0.020 <br /> <br />~. <br /> <br />., <br /> <br /> <br />",-,. <br />
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