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<br />~ <br />~,. <br />~ <br />~~ <br />1wII <br />,;11 <br />,.. <br />1~ <br />~" <br />~. <br />~II <br />'III <br />... <br />~~ <br />Irll <br />tr" <br />'r~ <br />frJ' <br />~, <br /> <br />Meetings were held by the Colorado Water Conservation Board with the Colorado Department of <br />Transportation (CDOT) to discuss the feasibility of widening the existing highway bridges. Because <br />the northbound bridge is an existing wood structure it cannot be widened; therefore, total replacement <br />would be necessary. <br /> <br />Three alternatives were investigated to resolve the problem of the undersized bridges at HWY 6. <br />Alternative 1 involves the removal and replacement of existing timber bridge along the northbound <br />lanes. The Colorado Department of Transportation (CDOT) currently has plans to replace the timb'~r <br />bridge within the next 3 to 5 years. For the southbound lanes, the existing concrete bridge would be <br />widened to convey the I DO-year peak discharge. <br /> <br />Alternative 2 involves adding box culverts just south of the existing bridges in lieu of widening or <br />replacing them. Based on a cursory evaluation, it was determined that four 20' x 8' concrete box <br />culverts would be required in addition to the existing bridges to convey the 1 DO-year peak discharge. <br />The culverts would be placed adjacent to and south of the existing blidge structure. <br /> <br />Alternative 3 investigated utilizing an existing railroad bridge crossing Structure which is located <br />approximately 1,500 feet north of the Pawnee Creek crossing. The: highway crossing at this location <br />has two existing concrete box culverts (3' x lO') which carry some local flows under the highway and <br />through an existing railroad blidge. The railroad bridge opening is fairly large (approximately 5' x <br />1 13') and would carry a larger flow than we highway crossing. Alternative 3 would require initial <br />flood flows 011 Pawnee Creek to be conveyed through the existing highway and railroad bridges along <br />the main channel. Once the capacity of these structures is reached, overflows would be conveyed by a <br />system of levees to the crossing 1,500 feet north. At this location, HWY 6 would be depressed to ac: <br />as an overflow weir and the flood flows would overtop the highway and be conveyed through the <br />existing railroad blidge. A system of additional levees would be required dO"'l1stream to confine the <br />flood flows to the South Platte River 1 DO-year floodplain. <br /> <br />Cursory evaluations completed for this alternative proved it not to be feasible. Evaluations showed <br />that only about half of the 100-year flood event (4,lOO cfs) could be cOll\'eyed through the existing <br />Pa\\l1ee Creek bridges; therefore, overflows to the north would be on the order of about 4, 1 00 cfs. <br />Depressing HWY 6 to pass the flows would require a length of about l,200 to 1,400 feet in order to <br />meet CDOT design criteria. With a weir letlgth this long. flows overtopping the highway would be <br />very wide and could not get back into the existing charUlel in order to be conveyed through the railroad <br />bridge. Additionally, because of the adjacent topography and elevation of the highway. the flood <br />control levees cannot be constructed high enough to provide 3 feet of freeboard. Therefore, FEMA <br />criteria could not be met and removal of the flood prone areas along the Pawnee Creek Overflow <br />would be difficult. Based on the cursory review of Altemative 3, it was not studied filrther. <br /> <br />Plan Description <br /> <br />lOO-Year Residual Floodplain: The results of the hydraulic analysis show that by eliminating the split <br />flows at channel station 224+00, the I DO-year water surface elevations will increase by I to :2 feet from <br />channel station 125+00 to channel station 214+00. This increase in the water surface elevation will <br />cause the floodplain to inundate a wider area to the south and flood a low lying area between channel <br />stations 168+00 and 224+00. There may also be additional shallow Hooding to the south of Pav,l1ee <br />Creek between stations 144+00 and 168+00. Bowever, based the existing mapping (scale of I" = 800' <br />and a 5 foot contour interval) it is difficult to be certain that this flooding will occur. <br /> <br />,~ <br />~L <br />