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Sediment Pond lit <br />• T[ethod 1 - Peak Floe Daing Te vs. CSIS Charts: <br />Hote: Time of eoaeentration (Te) may be computed ucing either travel <br />time or lag as show below. (There are other methods used to <br />obtain Tc which mey be preferred over the ones •how below.) <br />A• Computation of Tc Using Travel Time <br />Page 2 of 4 <br />Te .Length of Segment (Li) ~ Ll + L2 + L; + ...Ln x 1 <br />Velocity Through Segmen[ (Vi) Vl V2 V3 Va 3600 ~ Hrs. <br />• <br />LI~Ft. Vi~Ft/See. <br />B• Computation of Tc Usinq Lag 1/ <br />Slope Data: Watershed Height (z) 410 ft. <br />Contour Length (LC 25) .2400 -ft. X255 of (z) <br />Contour Length (LCSO) ~ 324~_~t. @505 of (;) <br />Contour Length (LC75) ~ 81 ft. @755 of (z) <br />Drainage Area (DA) ~ 2.018,570 <br />--esq. ft. <br />.25z(LC25 + LC50 + u7S) <br />Slope ~ x 1005 <br />DA (sq. ft.) <br />Aydraulie Length or Flov Length <br />Slope Y.ydraulic Soil Cover La <br />g Tc (hr) <br />(5) Length <br />(f t) Complex Y.o. (Equation <br />3.2) (1.667 x <br />Col. 4) <br />(1) 2 (3) 4 5 <br />32.75 3330 77 0.16 0.27 <br />C. Peak Flou <br /> <br />Te <br />(hr) <br />1 Peak Discharge <br /> <br />(FS 5 ) <br />2 <br />Total Area <br />(sq. mi.) <br />(3) Storm <br />requeney <br />(yr.) <br />(4) <br />P.unoff <br />(in.) <br />5 Total Peak <br />Discharge (cfs) <br />(Co1.2 x 3 x 5) <br /> 0.02 10 0.56 28.38 <br /> <br /> <br /> <br />1/ Intended for watersheds in theiz natural condition. If SSgniflcant <br />urbih areas exact use Page 4 for modlfieatfon. <br />32.75 5 <br />3330 ft. <br />• <br />