Laserfiche WebLink
<br />Table 1 TR-20 Schematic Information <br />-------------------------------------------------------------- <br />Seo IO " Area eN To Reach Information <br />From To Sq .i "" Length-Ft x m <br />-----------------------------------------~-------------------- <br />52 222.36 " 13.13 <br />" 131.82 " 11.97 <br />" " 43700 0.18 1.33 <br />" 61.65 " 8.71 <br />" " 15400 0.05 1.33 <br />" 71.63 " 9.77 <br />" " 42000 0.10 1.33 <br />" 81.69 " 10.94 <br />" " 48700 0.18 1.33 <br />" 58.35 " 11.34 <br />" " 36000 0.18 1.33 <br />" " 9500 0.18 1.33 <br />" " 9500 0.18 1.33 <br />" " 16300 0.10 1.33 <br />" " 25200 0.10 1.33 <br />" " 9200 0.18 1.33 <br />" 10 17400 0.18 1.33 <br />" 11 10900 0.18 1.33 <br /> <br />-------------------------------------------------------------- <br /> <br />11 <br /> <br />" <br /> <br />- <br /> <br />A major division of flow occurs between Country Road 31 and the <br />Pawnee Ditch crossing. The Pawnee Creek channel at this location <br />has very limited carrying capacity. A portion of channel <br />overflow moves overland in a southeasterly direction for about 2 <br />miles to U.S. Highway 6 at a location southwest of Atwood. The <br />highway and Burlington Northern Railroad redirect the flow <br />northeast through Atwood and on toward the Pawnee Creek highway <br />and railroad bridges. However, about a mile before the flow <br />reaches the main highway bridge, a restricting ridge causes <br />overflow across the highway and railroad towards the nearby South <br />Platte River. The remainder of this flow continues on to the <br />main highway bridge where it combines with flows from the main <br />channel and adjacent flood plain. <br />The main highway and railroad bridges on Pawnee Creek and the <br />overflow bridges about 1000 ft further down the highway to the <br />northeast toward Sterling will not accommodate the lOO-year flow <br />reaching this point. Therefore, some water will continue to the <br />northeast along the highway beyond the bridges towards the <br />Riverside Cemetery. <br />Another segment of out-of-bank flow occurs along the main channel <br />just downstream from County Road 33. This segment of flow moves <br />overland away from the main channel towards the northeast and <br />eventually to the vicinity of the Riverside Cemetery. This flow <br />combines with the residual overflow from the main channel highway <br />and railroad bridges" The consolidation occurs at a location <br />along U.S. Highway 6 near the Riverside Cemetery. It appears <br />additional flood water moves across the highway and railroad at <br />this location with some continuing on past the cemetery towards <br />Sterling. <br /> <br />Flows that pd"''' through tho< highway and railn,ad b."ldges on the <br />main stem of Pawnee Creek encounter alluvial fan type topography <br />in the vicinity of a farmstoad immediately below the railroad. A <br />three way division of flow occurs here with about 440 cr", <br />remaining in the channel and the balance going out-of-bank <br />splitting to the northeast and the south. <br />The following table, Figure 2, and Figure 3 show the location and <br />magnitude of flood flows, including their divisions and <br />combining, throughout the study reach. <br /> <br />-------------------------------------------------- <br /> <br />Location <br /> <br />Discharge - cfs <br />10 yr 25 yr SO yr <br /> <br />100 yr <br /> <br />-------------------------------------------------- <br /> <br />Highway 14 <br />Gounty il<! '.5 <br /> <br />12200 <br />11400 <br /> <br />7300 <br />6700 <br /> <br />9600 <br />8900 <br /> <br />4700 <br />4300 <br /> <br />-------------------------------------------------- <br />