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C <br />Sedimenc Pond lil Pit Component <br />Method 1 - peak Flw Using Te va. CSlI Charts: <br />Hote: Time of concentration (Tc) may be computed using d ther travel <br />time or leg as shown below. (There are other methods used to <br />obtain to which may be preferred over the ones show below,) <br />A• Computation of Tc Using Travel Time <br />Page 2 of <br />Te -Length of Segment (Li) - Ll + L2 + L3 + ...Ln : 1 - Ars. <br />Velocity Through Segment (Vi) 01 p2 p3 Vn 3600 <br />Li-Ft. VS-FtJSee. <br />$• Computation of Tc Using Lag I/ <br />Slope Data: Watershed Aelght (z) - - <br />Contour Length (LC25) <br />Contour Length (LC50) <br />Contour Length (LC75) <br />Drainage Area (DA) - 11, <br />940 ft. <br />- 7250 -ft. ~25~ of (z) <br />- 5250 ft, @SOS of (;) <br />3550 ft. @75x of (z) <br />456,280 <br />--esq. ft. <br />.25z(LC25 + LCSO + LC75) <br />Slope - x 1001 - 32.92 X <br />DA (sq• ft.) 8700 ft. <br />Hydraulic Length or Flov Length - <br />• <br />dope Y.ydraulie <br />Soil Cover ~ <br />Lag Tc (hr) <br />~ <br />(y) Len th <br />(fi) <br />Complex !!o. <br />(Equation 3.2) (1.667 x <br /> <br />(1) <br />2 <br />(3) Col. 4) <br /> 4 5 <br />32.92 8700 84 0.27 0.46 <br />C. Peak Flog: <br />Tc <br /> <br />(hr) <br />1 Peak Discharge <br />cfs/in./sq.mi.) <br />(Ff 5-1) <br />2 <br />Total Area <br />(s q. mi.) <br />(3) Stotm <br />requeney <br />(yr.) <br />(4) <br />Runoff <br />(in.) <br />5 Total Peak <br />Discharge {cfs) <br />(Col. 2x3x5) <br />0.46 525 0.41 10 yr. 0.89 191.57 <br /> <br /> <br /> <br />1/ Intended for vacersheds in their natural condition. If SSgnifieant <br />urbah areas exist use Page G for modification. <br /> <br />