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<br />I <br />'I <br />I <br /> <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 />II <br />I <br />I <br />I <br />I <br /> <br />HYDRAULIC ANALYSIS <br /> <br />Analysis of the hydraulic characteristics ofthe study reach of the Cache La Poudre River was <br />carried out to provide estimates of the water surface elevations of floods at the selected <br />recurrence intervals. The water surface elevations were computed through use of a hydrologic <br />and hydraulic software program, which is compatible with the Corps of Engineers HEC-2 step- <br />backwater computer program. Cross sections for the analysis of the Poudre River were obtained <br />from digitized cross sections of a topographic map for the area and field survey. <br />Channel roughness factors (Manning's "n") for these computations were assigned on the basis <br />of field inspection of the floodplain areas and check for consistency with values used in other <br />previous studies. Manning's values range from 0.03 to 0.05. <br />Average velocities in the floodplain range from 9,8 to 13.1 feet per second, while average <br />velocities for the floodway range from 9.8 to 13.2 feet per second, Scour holes do occur under <br />both of the bridges. This is a common occurrence and in some cases scour holes can be several <br />feet deep. Cross section data from the topographic mapping was adjusted for actual stream bed <br />elevations under the bridges where scour had occurred. <br />Scour holes under and near bridge structures in most cases continue under the entire bridge <br />and increase the hydraulic capacity of the structure slightly; therefore these depressions were <br />considered in the hydraulic analysis. These scour holes are a result of flood events that have <br />occurred before in this area, but do not appear to be filling with sediment during low-flow <br />periods. <br />Details of the hydraulic analysis is included in the Technical Addendum, <br /> <br />6 <br />