Laserfiche WebLink
River Sedimentation Pond design is set forth since they <br />relate to emergency spillway design. <br />• Drainage Area =1.29 acres <br />Curve Number BO <br />Hydrologic Group D <br />Precipitation <br />10 year 24 hour event 1.6" <br />25 year 24 hour event 2.0" <br />100 year 24 hour event 2.6" <br />Peak Flow Calculations <br />Unadjusted peak runoff factor Peak flow = 3.2cfs <br />a10 a25 0100 010 025 x100 <br />.34" .56" .96" 1.12 1.85 3.16 <br />Total Flow Calculations <br />Drainage Area, Da = 1.29 acres <br />Total O10 (.34) 1.29 acres x. 34"/12in/ft = .04ac/ft <br />Total 025 (.56) 1.29 acres x .56"/12in/ft = .06ac/ft <br />Total 0100(.96) 1.29 acres x .96"/12in/ft = .l0ac/ft <br />Design sedimentation pond to contain 10 year 24 hour <br />storm, include sediment storage = .Olac/ft <br />Construct impoundment total volume .O5ac/ft: 5 feet <br />deep; 3 horizontal: 1 vertical sideslopes: triangular <br />shape, 3o feet wide x 30 feet long; dewatering device <br />must convey 0100 = 3.16 cfs. <br />Install 18 inch capable to convey 5.Scfs with CMP <br />Project-no head. <br />• A review of the as built Yampa River Sedimentation Pond <br />computations in my lOJuly90 report are as follows: <br />Total volume =0.537acft <br />Computations: <br />Area of embankment break in slope (measured) <br />57 x 103 = 5871 5871 x 0.95 =5577sgf~ <br />Area at top of dewatering device (calculated) <br />51.4 x 95 = 4883 4883 x 0.95 =4639sgft <br />Area at waterline (measured) <br />38.5 x 82 = 3157 3157 x 0.95 =2999sgft <br />Area at pond bottom (calculated) <br />20.4 x 67.3 = 1373 1373 x 0.95 =1304sgft <br />Volume from embankment break-in-slope <br />to waterline <br />0.5(2999+5577) x 3.95 = 16938cuft =0.389acft <br />Volume of water <br />0.5( 1304+2999) x 3(estimated)=6455cuft <br />or =0.148acft <br />Total =0.537acft <br />The accompanying graph, Yampa River Sedimentation Pond <br />Storage Capacity, utilizes three control points for the <br />graph plot: zero storage; depth and volume of water on <br />4June90; and depth and total volume to embankment break-in- <br />slope. The line is curvilinear due to the irregular <br />• trapezoidal pond shape, and estimates regarding water depth <br />and projections of bank inclinations. None the less, plots <br />~~~ I <br />