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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 />. <br />I <br /> <br />basin contains 711 acres (1.11 square miles) and extends from the confluence to 1-25 just <br /> <br /> <br />north of 112th Avenue. The sub-basin lies entirely within the City of Northglenn. <br /> <br /> <br />The major features of the basin are Washington Street, 112th Avenue, Irma Drive, <br /> <br /> <br />the Union Pocific Railrood embankment, ond the Northglenn Municipal facilities. The <br /> <br /> <br />water course above the Union Pacific Railroad consists of overland, street, and storm <br /> <br /> <br />sewer flow. Below the Union Pacific Railroad a well-defined open chonnel carries the <br /> <br /> <br />storm flows to Grange Hall Creek. <br /> <br />C. Basin Hydroloqy <br /> <br />The next step in the hydrologic analysis was to define the runoff peak flows and <br /> <br /> <br />volumes for the existing and future developed conditions for eoch of the sub-basins and <br /> <br /> <br />then combine the flows to define the design runoff at the desired hydrologic points. These <br /> <br /> <br />design flows were subsequently used to define the different flood plains and thence <br /> <br />potential droinage problem areas. <br />I. Sub-basin Characteristics <br /> <br />5. Tributary SE <br />The smallest of the sub-basins (that is part of the major droinageway plonning) is <br />Tributary SE, which is a right bank tributary to Grange Hall Creek approximotely one- <br />quarter mile above Riverdale Rood. The sub-basin contains 141 acres (0.22 squore miles) <br />and extends from the confluence to just east of York Street along 104th Avenue. The area <br />above the Union Pacific Railroad lies within Tharnton. From the Union Pacific Railroad <br /> <br />The entire study area was divided into 44 sub-basins ranging in size from 37 acres to <br /> <br /> <br />395 acres (see Figure 111-1 and Table III-I). The rather detailed basin division was <br /> <br />considered necessary to adequately define the runoff at the various hydrologic points and <br />to account for the effects of basin development, channelization, and stream detention on <br />the runoff characteristics in the various channels using the U.D. and F.C.D. runoff <br />modeling techniques. <br /> <br />to Colorodo Blvd. the sub-basin lies within Adams County. Below Colorado Blvd. the sub- <br /> <br />For each of the sub-basins the area, length, centroid length, slope, percent <br /> <br /> <br />imperviousness, Cp and Ct values were determined for the existing and future <br /> <br /> <br />development conditions with existing drainage facilities. The parameters for the existing <br /> <br /> <br />development were determined fro'n aerial photos provided by the District and Northglenn, <br /> <br /> <br />and from field inspection of the basin. The future development para:neters were defined <br /> <br />basin ogoin comes under the jurisdiction of Thornton. <br /> <br />The major features of the bosin are the Union Pacific Railroad, Colorado Blvd., <br /> <br /> <br />Brewer Reservoir, and the Colorado Agricultural Canal. The channel above the Union <br /> <br /> <br />Pacific Railroad is mainly overland flow due to the lack of development. Between the <br /> <br /> <br />Union Pacific Roilroad and Colorado Blvd. the woter course consists of broad V-type <br /> <br /> <br />channel. Just to the east of Colorado Blvd. Brewer Reservoir has been constructed with a <br /> <br />by utilization of the future land use map. <br /> <br />high embankment. Between the pond and the Colorado Agricultural Canal there exists a <br /> <br /> <br />brood V-type channel, which essentially disoppears below the canal. The actual woter <br /> <br />In addition to the above-listed characteristics, the storm sewer drainage density was <br /> <br /> <br />determined for each sub-basin. The storm sewer drainage density is defined as the lineal <br /> <br /> <br />feet of storm sewer per acre of land, and is used to determine the degree that the basin is <br /> <br />towards 104th Avenue, then east along 104th Avenue and into the Colorodo Agricultural <br />Conal. The overflow from the canal then flows northeasterly into Grange Hall Creek. <br /> <br />sewered so that the Cp and Ct parameters con be modified. The amount of sewer length <br /> <br /> <br />in each sub-basin was determined from the storm sewer maps of Northglenn and field <br /> <br />course is not within the channel, since the emergency overflow from the pond is south <br /> <br />investigations. <br /> <br />9 <br />