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I <br />180)' <br />3.2.3 Hydraulic Modeling <br />Numerical hydraulic models were assembled for each of the problem areas to analyze <br />current conditions. The HEC -2, Water Surface Profiles program (USACE 1990) was used for <br />hydraulic analysis. This program is applicable to steady, gradually varied flow conditions. It <br />was assumed that the controlling hydraulic conditions were represented within the boundaries of <br />the geometry provided, i.e., that conditions downstream of the areas would not substantially <br />influence the profiles within the computer models. The downstream boundary condition was <br />calculated using the Slope -Area method. Cross- section geometry was obtained from Digital <br />Terrain Modeling (DTM) provided by Kucera International, Inc., under contract to CWCB. <br />Reach lengths between cross - sections along the channel were generated when the cross - sections <br />were extracted. The overbank reach lengths were scaled from the orthophotos. The State <br />Highway 109 Bridge was modeled according to dimensions provided by the State. Manning's <br />"n" roughness values were assigned based on a combination of previous studies, field conditions, <br />sediment transport theory, and engineering judgement. The specific "n" values for the individual <br />problem areas are shown in Table 3 -4. Contraction and expansion coefficients used were 0.1 and <br />0.3, respectively. <br />Table 3 -4. Manning's roughness values. <br />Problem Area <br />Left Overbank <br />Channel <br />Right Overbank <br />1 <br />0.030 -0.090 <br />0.025 <br />0.030 -0.070 <br />2 <br />0.030 -0.070 <br />0.025 <br />0.030 -0.070 <br />3 <br />0.035 -0.070 <br />0.025 <br />0.035 -0.070 <br />Flows of 100, 200, 300, 500, 750, and 1,000 cfs were modeled to indicate channel capacities and <br />potential problem areas under current conditions. Most areas had a channel capacity of less than <br />1,000 -cfs. <br />There were numerous problems with the lack of topographic detail between cross - sections in <br />determining the location of the channel banks as well as the overbank areas. Therefore, we <br />estimated bank locations using the "Edith2" program and measuring the approximate channel <br />widths on the orthophotos. <br />3.2.4 Sediment Analysis <br />Sedimentation was analyzed using Hydraulic Design Package for Channels (USACE <br />1997), also known as SAM. This is an integrated system of programs developed to aid engineers <br />in analyses associated with designing, operating, and maintaining flood control channels and <br />stream restoration projects. SAM provides the computational capability to include erosion, <br />entrainment, transportation, and deposition of sediment in channels. The hydraulic, sediment <br />transport and sediment yield modules of the program were used in this study. <br />31 <br />