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Last modified
1/25/2010 7:08:13 PM
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10/5/2006 2:05:54 AM
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State of Colorado
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Title
Measurment of Peak Discharge at Culverts by Indirect Methods
Date
6/1/1968
Prepared By
G.L. Bodhaine
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br /> <br />- <br /> <br />e- <br /> <br />-; <br /> <br />e <br /> <br />MEASUREMENT OF PEAK DISCHARGE A T CULVERTS BY INDIRECT METHODS <br /> <br />By G. L. Bodhai"" <br /> <br />-, <br />" <br />" <br />" <br />" <br />',N. V22 <br />r 2~__ <br /> <br />I ----- <br />D ----_ Water <br />L --__~u~:c::._ <br /> <br />Abstract <br /> <br />This chapter classifies culvert flow into six types, <br />gives discharge equations based on continuity and <br /><'nergy equations, and describes procedures for meas- <br />uring peak discharges llsing culverts in the field. Di8. <br />charge coefficients for n variety of geometries and flow <br />t.ypes 1\n' given. Tl'll mmmph'51 detail stf>p-by-step <br />computation procedurc~. <br /> <br />Introduction <br /> <br />The peak discharge through culverts can be <br />determined from high-wuter marks that define <br />the headwater and tailwuter elevations. This <br />indirect method is used extensively to measure <br />flood discharges from small drainage areas. <br />The head-discharge characteristics of cul- <br />"erts have been studied in laboratory inves- <br />tigations by the U .S, Geological Survey, the <br />Bureau of Public Roads, and many universities. <br />The procedures given in this report are based <br /> <br />VI' <br />02"9--= <br /> <br />FG[ 11'1-2 <br /> <br />Entrance loss <br /> <br />h, <br /> <br />z <br /> <br />(I) <br />Approach <br />section <br /> <br />(2) <br />Culvert <br />entrance <br /> <br />on the information obtained in these studies <br />and in field studies of the flow through culverts <br />at sites where the discharge was known, <br /> <br />Description of Culvert Flow <br /> <br />The placement of a roadway fill and culvert <br />in a stream channel causes an abrupt change <br />in the character of flow, This channel transition <br />results in rapidly varied flow in which aceelera- <br />tion rather than boundary friction plays the <br />primary role. The flow in the approach channel <br />to the culvert is usually tranquil and fairly <br />uniform. Within the culvert, however, the flow <br />may be tranquil, critical, or rapid if the culvert <br />is partly filled, or the culvert may flow full <br />under pressure. <br />The physical features associated with cul- <br />vert flow are illustrated in figure 1. They are <br />the approach channel cross section at a distance <br />equivalent to one opening width upstream from <br /> <br />Energy grade line <br />Top culvert <br /> <br />I <br />h,i-J <br /> <br />--- <br /> <br />V,, <br />~29 <br />-----i--r- <br />d3 "4 <br /> <br />Bottom culvert <br />Datu <br /> <br />/(3) (4) <br />Culvert Ta iI water <br />outlet section <br /> <br />Figure 1.-Definition-sketch of culvert flow. Note.-The loss .of energy neat the entrance is related to the sudden <br />contraction and subsequent expansion of the lin stream within the culvert bane!. <br /> <br />1 <br /> <br />/' <br />
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