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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />calculated to be 1,500 cfs. The 100-year existing condition discharge in Tri-Area Drainageway <br />at !VCR 13 is 2,590 cfs, <br />WC:R 16 C:ulvert The crossing at WCR 16 is a 6'H x 10'W reinforced concrete box <br />culvert. At this location, overtopping of the right bank and associated flooding of adjacent <br />property and WCR 16, occurs 50 feet upstream at a depth of approximately 10.3 feet above the <br />invert of the culvert. The capacity of the culvert prior to overtopping is 710 cfs, The 100-year <br />existing condition discharge in Tri-Area Drainageway at WCR 16 is 1,940 cfs. <br />Main Street Frederick Culvert The crossing at Main Street is a 6'H x 8'W reinforced <br />concrete box culvert. At this location, overtopping of the right bank occurs at the upstream face <br />. of the culvert, at a depth of approximately 8.6 feet above the invert. The capacity of the culvert <br />prior to overtopping is 520 cfs, The lOa-year existing condition discharge in Tri-Area <br />Drainageway at Main Street is 1,940 cfs, <br />State Higbway 52/Eighth Street C:ulverts. This crossing of State Highway 52 and Eighth <br />Street in Dacono is comprised of a cluster of corrugated metal pipes. Two CMPs with diameters <br />of 3.5 feet and 4,0 feet convey flow under Eighth Street. One 3.5-foot CMP and two arched <br />CMPs (2.5'H x 4'W) convey flow under State Highway 52, At this location, roadway <br />overtopping occurs at a depth of approximately 6.0 feet from the invert of the most upstream <br />culvert, Due to the potential debris loading, all of these pipes were assumed to be ineffective <br />during large events, The lOO-year existing condition discharge in Tri-Area Drainageway at State <br />Highway 52 is 1,520 cfs, <br /> <br />3.3 Open Channels <br /> <br />3.3.1 Godding Hollow Rasin <br /> <br />At WCR 24V2, the Godding Hollow major drainageway confluences with the Rural Ditch. <br />Stormwater runoff within the Godding Hollow channel combines with the water conveyed in the <br />Rural Ditch and continues northeast for approximately 1,800 feet before emptying into the Rural <br />Ditch Wasteway at the end of the Rural Ditch. This reach of the Rural Ditch is incapable of <br />conveying stormwater runoff from even minor storm events within the Godding Hollow Basin. <br />Similarly, the other irrigation ditches, namely the Coalridge Ditch, Godding Ditch, and the Last <br />Chance Ditch, offer limited value as drainage features that will capture and convey stormwater out <br />of the basin. Furthermore, the major drainageway of the Godding Hollow Basin is typically <br />incapable of conveying stormwater runoff generated from any event in excess' of the 2-year <br />existing condition storm event. <br /> <br />T:iOPEMCoweldO/\CoweldOJ Inl rpt.wpd <br /> <br />3.10 <br /> <br />Septernber8,1999 <br />